386:. In that case, the ice sheet may not be thinning at all, as the amount of ice flowing over the grounding line would be likely to match the annual accumulation of ice from snow upstream. Otherwise, ocean warming at the base of an ice shelf tends to thin it through basal melting. As the ice shelf becomes thinner, it exerts less of a buttressing effect on the ice sheet, the so-called back stress increases and the grounding line is pushed backwards. The ice sheet is likely to start losing more ice from the new location of the grounding line and so become lighter and less capable of displacing seawater. This eventually pushes the grounding line back even further, creating a
1306:
1100:
484: ft) in basal (underground) height are likely to collapse under their own weight once the peripheral ice stabilizing them is gone. Their collapse then exposes the ice masses following them to the same instability, potentially resulting in a self-sustaining cycle of cliff collapse and rapid ice sheet retreat - i.e. sea level rise of a meter or more by 2100 from Antarctica alone. This theory had been highly influential - in a 2020 survey of 106 experts, the paper which had advanced this theory was considered more important than even the year 2014
38:
1386:
1444:, the northern hemisphere warmed considerably, dramatically increasing the release of methane from wetlands, that were otherwise tundra during glacial times. This methane quickly distributes evenly across the globe, becoming incorporated in Antarctic and Greenland ice. With this tie, paleoclimatologists have been able to say that the ice sheets on Greenland only began to warm after the Antarctic ice sheet had been warming for several thousand years. Why this pattern occurs is still open for debate.
732:
532:
170:
399:
1554:
1462:
9644:
214:
9632:
281:
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9656:
427:
near future, although the dynamic behavior of Totten Ice Shelf is known to vary on seasonal to interannual timescales. The Wilkes Basin is the only major submarine basin in
Antarctica that is not thought to be sensitive to warming. Ultimately, even geologically rapid sea level rise would still most likely require several millennia for the entirety of these ice masses (WAIS and the subglacial basins) to be lost.
939:
222:
268:. These lakes may feed warm water to glacial bases and facilitate glacial motion. Lakes of a diameter greater than ~300 m are capable of creating a fluid-filled crevasse to the glacier/bed interface. When these crevasses form, the entirety of the lake's (relatively warm) contents can reach the base of the glacier in as little as 2–18 hours – lubricating the bed and causing the glacier to
1065:. Those areas are sometimes collectively described as East Antarctica's subglacial basins, and it is believed that once the warming reaches around 3 °C (5.4 °F), then they would start to collapse over a period of around 2,000 years, This collapse would ultimately add between 1.4 m (4 ft 7 in) and 6.4 m (21 ft 0 in) to sea levels, depending on the
436:
5331:
impact, locally as the radiative forcing from greenhouse gases. The temperature change in any particular region will in fact be a combination of radiation-related changes (through greenhouse gases, aerosols, ozone and the like) and dynamical effects. Since the winds tend to only move heat from one place to another, their impact will tend to cancel out in the global mean.
260:, an ice stream will remain almost stationary for hours at a time, before a surge of around a foot in under an hour, just after the peak high tide; a stationary period then takes hold until another surge towards the middle or end of the falling tide. At neap tides, this interaction is less pronounced, and surges instead occur approximately every 12 hours.
571:- did not resemble predictions from ice cliff collapse at least up until the end of 2013, but an event observed at Helheim Glacier in August 2014 may fit the definition. Further, modelling done after the initial hypothesis indicates that ice-cliff instability would require implausibly fast ice shelf collapse (i.e. within an hour for ~90 m (
371:. Effectively, these marine ice sheets must have enough mass to exceed the mass of the seawater displaced by the ice, which requires excess thickness. As the ice sheet melts and becomes thinner, the weight of the overlying ice decreases. At a certain point, sea water could force itself into the gaps which form at the base of the ice sheet, and
7420:
Woodward, John; Winter, Kate; Weyrich, Laura S.; Rootes, Camilla M.; Millman, Helen; Albert, Paul G.; Rivera, Andres; Ommen, Tas van; Curran, Mark; Moy, Andrew; Rahmstorf, Stefan; Kawamura, Kenji; Hillenbrand, Claus-Dieter; Weber, Michael E.; Manning, Christina J.; Young, Jennifer; Cooper, Alan (25 February 2020).
6422:
Briner, Jason P.; Cuzzone, Joshua K.; Badgeley, Jessica A.; Young, Nicolás E.; Steig, Eric J.; Morlighem, Mathieu; Schlegel, Nicole-Jeanne; Hakim, Gregory J.; Schaefer, Joerg M.; Johnson, Jesse V.; Lesnek, Alia J.; Thomas, Elizabeth K.; Allan, Estelle; Bennike, Ole; Cluett, Allison A.; Csatho, Beata;
1202:
is an ice sheet which forms the second largest body of ice in the world. It is an average of 1.67 km (1.0 mi) thick, and over 3 km (1.9 mi) thick at its maximum. It is almost 2,900 kilometres (1,800 mi) long in a north–south direction, with a maximum width of 1,100 kilometres
5456:
Although their methods of interpolation or extrapolation for areas with unobserved output velocities have an insufficient description for the evaluation of associated errors, such errors in previous results (Rignot and others, 2008) caused large overestimates of the mass losses as detailed in Zwally
6228:
Christ, Andrew J.; Bierman, Paul R.; Schaefer, Joerg M.; Dahl-Jensen, Dorthe; Steffensen, Jørgen P.; Corbett, Lee B.; Peteet, Dorothy M.; Thomas, Elizabeth K.; Steig, Eric J.; Rittenour, Tammy M.; Tison, Jean-Louis; Blard, Pierre-Henri; Perdrial, Nicolas; Dethier, David P.; Lini, Andrea; Hidy, Alan
915:
could stabilize them, but it would be extraordinarily difficult and may not account for the ongoing acceleration of ocean warming in the area. Others suggest that building obstacles to warm water flows beneath glaciers would be able to delay the disappearance of the ice sheet by many centuries, but
891:
period, when the global temperatures were similar to the early 21st century. It is believed that the loss of the ice sheet would take place between 2,000 and 13,000 years in the future, although several centuries of high emissions may shorten this to 500 years. 3.3 m (10 ft 10 in) of
426:
is the largest glacier there which is known to be subject to MISI - yet, its potential contribution to sea level rise is comparable to that of the entire West
Antarctic Ice Sheet. Totten Glacier has been losing mass nearly monotonically in recent decades, suggesting rapid retreat is possible in the
234:
Even stable ice sheets are continually in motion as the ice gradually flows outward from the central plateau, which is the tallest point of the ice sheet, and towards the margins. The ice sheet slope is low around the plateau but increases steeply at the margins. This difference in slope occurs due
1281:
If all 2,900,000 cubic kilometres (696,000 cu mi) of the ice sheet were to melt, it would increase global sea levels by ~7.4 m (24 ft). Global warming between 1.7 °C (3.1 °F) and 2.3 °C (4.1 °F) would likely make this melting inevitable. However, 1.5 °C
293:
188:
have a much greater area than this minimum definition, measuring at 1.7 million km and 14 million km, respectively. Both ice sheets are also very thick, as they consist of a continuous ice layer with an average thickness of 2 km (1 mi). This ice layer forms because most of the snow which
1433:
are abrupt warmings of the northern hemisphere occurring over the space of perhaps 40 years. While these D–O events occur directly after each
Heinrich event, they also occur more frequently – around every 1500 years; from this evidence, paleoclimatologists surmise that the same forcings may drive
6729:
Christ, Andrew J.; Rittenour, Tammy M.; Bierman, Paul R.; Keisling, Benjamin A.; Knutz, Paul C.; Thomsen, Tonny B.; Keulen, Nynke; Fosdick, Julie C.; Hemming, Sidney R.; Tison, Jean-Louis; Blard, Pierre-Henri; Steffensen, Jørgen P.; Caffee, Marc W.; Corbett, Lee B.; Dahl-Jensen, Dorthe; Dethier,
346:
The collapse of the Larsen B shelf was preceded by thinning of just 1 metre per year, while some other
Antarctic ice shelves have displayed thinning of tens of metres per year. Further, increased ocean temperatures of 1 °C may lead to up to 10 metres per year of basal melting. Ice
5330:
At first glance this seems to contradict the idea of "global" warming, but one needs to be careful before jumping to this conclusion. A rise in the global mean temperature does not imply universal warming. Dynamical effects (changes in the winds and ocean circulation) can have just as large an
5015:
Galeotti, Simone; DeConto, Robert; Naish, Timothy; Stocchi, Paolo; Florindo, Fabio; Pagani, Mark; Barrett, Peter; Bohaty, Steven M.; Lanci, Luca; Pollard, David; Sandroni, Sonia; Talarico, Franco M.; Zachos, James C. (10 March 2016). "Antarctic Ice Sheet variability across the Eocene-Oligocene
7419:
Turney, Chris S. M.; Fogwill, Christopher J.; Golledge, Nicholas R.; McKay, Nicholas P.; Sebille, Erik van; Jones, Richard T.; Etheridge, David; Rubino, Mauro; Thornton, David P.; Davies, Siwan M.; Ramsey, Christopher Bronk; Thomas, Zoë A.; Bird, Michael I.; Munksgaard, Niels C.; Kohno, Mika;
1338:
There is a massive contrast in carbon storage between the two ice sheets. While only about 0.5-27 billion tonnes of pure carbon are present underneath the
Greenland ice sheet, 6000-21,000 billion tonnes of pure carbon are thought to be located underneath Antarctica. This carbon can act as a
4482:
Lau, Sally C. Y.; Wilson, Nerida G.; Golledge, Nicholas R.; Naish, Tim R.; Watts, Phillip C.; Silva, Catarina N. S.; Cooke, Ira R.; Allcock, A. Louise; Mark, Felix C.; Linse, Katrin (21 December 2023). "Genomic evidence for West
Antarctic Ice Sheet collapse during the Last Interglacial".
1296: ft) of sea level rise, and more ice will be lost if the temperatures exceed that level before declining. If global temperatures continue to rise, the ice sheet will likely disappear within 10,000 years. At very high warming, its future lifetime goes down to around 1,000 years.
226:
3295:
Horton, Benjamin P.; Khan, Nicole S.; Cahill, Niamh; Lee, Janice S. H.; Shaw, Timothy A.; Garner, Andra J.; Kemp, Andrew C.; Engelhart, Simon E.; Rahmstorf, Stefan (2020-05-08). "Estimating global mean sea-level rise and its uncertainties by 2100 and 2300 from an expert survey".
4534:
Armstrong McKay, David; Abrams, Jesse; Winkelmann, Ricarda; Sakschewski, Boris; Loriani, Sina; Fetzer, Ingo; Cornell, Sarah; Rockström, Johan; Staal, Arie; Lenton, Timothy (9 September 2022). "Exceeding 1.5 °C global warming could trigger multiple climate tipping points".
1015:
from the snow as well as the surface's consistently high elevation results in the reported cold temperature records of nearly −100 °C (−148 °F). It is the only place on Earth cold enough for atmospheric temperature inversion to occur consistently. That is, while the
223:
247:
but is controlled by temperature and the strength of individual glacier bases. A number of processes alter these two factors, resulting in cyclic surges of activity interspersed with longer periods of inactivity, on time scales ranging from hourly (i.e. tidal flows) to the
898:
The preservation of WAIS may require a persistent reduction of global temperatures to 1 °C (1.8 °F) below the preindustrial level, or to 2 °C (3.6 °F) below the temperature of 2020. Because the collapse of the ice sheet would be preceded by the loss of
1069:
used. The EAIS as a whole holds enough ice to raise global sea levels by 53.3 m (175 ft). However, it would take global warming in a range between 5 °C (9.0 °F) and 10 °C (18 °F), and a minimum of 10,000 years for the entire ice sheet to be
3440:
Edwards, Tamsin L.; Brandon, Mark A.; Durand, Gael; Edwards, Neil R.; Golledge, Nicholas R.; Holden, Philip B.; Nias, Isabel J.; Payne, Antony J.; Ritz, Catherine; Wernecke, Andreas (6 February 2019). "Revisiting
Antarctic ice loss due to marine ice-cliff instability".
5624:
Pan, Linda; Powell, Evelyn M.; Latychev, Konstantin; Mitrovica, Jerry X.; Creveling, Jessica R.; Gomez, Natalya; Hoggard, Mark J.; Clark, Peter U. (30 April 2021). "Rapid postglacial rebound amplifies global sea level rise following West
Antarctic Ice Sheet collapse".
441:
437:
2772:
Young, Duncan A.; Wright, Andrew P.; Roberts, Jason L.; Warner, Roland C.; Young, Neal W.; Greenbaum, Jamin S.; Schroeder, Dustin M.; Holt, John W.; Sugden, David E. (2011-06-02). "A dynamic early East
Antarctic Ice Sheet suggested by ice-covered fjord landscapes".
113:
Even stable ice sheets are continually in motion as the ice gradually flows outward from the central plateau, which is the tallest point of the ice sheet, and towards the margins. The ice sheet slope is low around the plateau but increases steeply at the margins.
438:
7385:
Bond, Gerard C.; Showers, William; Elliot, Mary; Evans, Michael; Lotti, Rusty; Hajdas, Irka; Bonani, Georges; Johnson, Sigfus (1999). "The North
Atlantic's 1–2 kyr climate rhythm: Relation to Heinrich events, Dansgaard/Oeschger cycles and the Little Ice Age".
1230:
for at least 18 million years, but a single ice sheet first covered most of the island some 2.6 million years ago. Since then, it has both grown and contracted significantly. The oldest known ice on Greenland is about 1 million years old. Due to anthropogenic
892:
sea level rise would occur if the ice sheet collapses but leaves ice caps on the mountains behind. Total sea level rise from West Antarctica increases to 4.3 m (14 ft 1 in) if they melt as well, but this would require a higher level of warming.
4291:; Xiao, C.; Aðalgeirsdóttir, G.; Drijfhout, S. S.; Edwards, T. L.; Golledge, N. R.; Hemer, M.; Kopp, R. E.; Krinner, G.; Mix, A. (2021). Masson-Delmotte, V.; Zhai, P.; Pirani, A.; Connors, S. L.; Péan, C.; Berger, S.; Caud, N.; Chen, Y.; Goldfarb, L. (eds.).
3906:
Barnett, Robert L.; Austermann, Jacqueline; Dyer, Blake; Telfer, Matt W.; Barlow, Natasha L. M.; Boulton, Sarah J.; Carr, Andrew S.; Creel, Roger (15 September 2023). "Constraining the contribution of the Antarctic Ice Sheet to Last Interglacial sea level".
2071:
Bell, R. E.; Ferraccioli, F.; Creyts, T. T.; Braaten, D.; Corr, H.; Das, I.; Damaske, D.; Frearson, N.; Jordan, T.; Rose, K.; Studinger, M.; Wolovick, M. (2011). "Widespread Persistent Thickening of the East Antarctic Ice Sheet by Freezing from the Base".
1389:
A reconstruction of how Heinrich events would have likely proceeded, with the Laurentide ice sheet first growing to an unsustainable position, where the base of its periphery becomes too warm, and then rapidly losing ice until it is reduced to sustainable
1031:. Clear warming over East Antarctica only started to occur since the year 2000, and was not conclusively detected until the 2020s. In the early 2000s, cooling over East Antarctica seemingly outweighing warming over the rest of the continent was frequently
6542:; Xiao, C.; Aðalgeirsdóttir, G.; Drijfhout, S.S.; Edwards, T.L.; Golledge, N.R.; Hemer, M.; Kopp, R.E.; Krinner, G.; Mix, A. (2021). Masson-Delmotte, V.; Zhai, P.; Pirani, A.; Connors, S.L.; Péan, C.; Berger, S.; Caud, N.; Chen, Y.; Goldfarb, L. (eds.).
2750:; Xiao, C.; Aðalgeirsdóttir, G.; Drijfhout, S.S.; Edwards, T.L.; Golledge, N.R.; Hemer, M.; Kopp, R.E.; Krinner, G.; Mix, A. (2021). Masson-Delmotte, V.; Zhai, P.; Pirani, A.; Connors, S.L.; Péan, C.; Berger, S.; Caud, N.; Chen, Y.; Goldfarb, L. (eds.).
418:
glaciers are most likely to be prone to MISI, and both glaciers have been rapidly thinning and accelerating in recent decades. As the result, sea level rise from the ice sheet could be accelerated by tens of centimeters within the 21st century alone.
7977:
Japsen, Peter; Green, Paul F.; Bonow, Johan M.; Nielsen, Troels F.D.; Chalmers, James A. (5 February 2014). "From volcanic plains to glaciated peaks: Burial, uplift and exhumation history of southern East Greenland after opening of the NE Atlantic".
225:
1402:(the amount of sunlight reaching the Earth). These patterns are caused by the variations in shape of the Earth's orbit and its angle relative to the Sun, caused by the gravitational pull of other planets as they go through their own orbits.
523:
period which appears consistent with MICI. However, it indicates "relatively rapid" yet still prolonged ice sheet retreat, with a movement of >200 km (120 mi) inland taking place over an estimated 1100 years (from ~12,300 years
1577:, which cover 76,000 and 100,000 square kilometres (29,000 and 39,000 sq mi) around the periphery. Conditions in Greenland were not initially suitable for a single coherent ice sheet to develop, but this began to change around 10
1619:, allowing ice to accumulate and persist. As recently as 3 million years ago, during the Pliocene warm period, Greenland's ice was limited to the highest peaks in the east and the south. Ice cover gradually expanded since then, until the
1268:
by the end of the century. If there are no reductions in emissions, melting would add around 13 cm (5 in) by 2100, with a worst-case of about 33 cm (13 in). For comparison, melting has so far contributed 1.4 cm
440:
263:
Increasing global air temperatures due to climate change take around 10,000 years to directly propagate through the ice before they influence bed temperatures, but may have an effect through increased surface melting, producing more
117:
Increasing global air temperatures due to climate change take around 10,000 years to directly propagate through the ice before they influence bed temperatures, but may have an effect through increased surface melting, producing more
1428:
Internal ice sheet "binge-purge" cycles may be responsible for the observed effects, where the ice builds to unstable levels, then a portion of the ice sheet collapses. External factors might also play a role in forcing ice sheets.
3831:
Crawford, Anna J.; Benn, Douglas I.; Todd, Joe; Åström, Jan A.; Bassis, Jeremy N.; Zwinger, Thomas (11 May 2021). "Marine ice-cliff instability modeling shows mixed-mode ice-cliff failure and yields calving rate parameterization".
6176:
Reyes, Alberto V.; Carlson, Anders E.; Beard, Brian L.; Hatfield, Robert G.; Stoner, Joseph S.; Winsor, Kelsey; Welke, Bethany; Ullman, David J. (25 June 2014). "South Greenland ice-sheet collapse during Marine Isotope Stage 11".
3402:
Gilford, Daniel M.; Ashe, Erica L.; DeConto, Robert M.; Kopp, Robert E.; Pollard, David; Rovere, Alessio (5 October 2020). "Could the Last Interglacial Constrain Projections of Future Antarctic Ice Mass Loss and Sea-Level Rise?".
5990:
Thiede, Jörn; Jessen, Catherine; Knutz, Paul; Kuijpers, Antoon; Mikkelsen, Naja; Nørgaard-Pedersen, Niels; Spielhagen, Robert F (2011). "Millions of Years of Greenland Ice Sheet History Recorded in Ocean Sediments".
5889:
Höning, Dennis; Willeit, Matteo; Calov, Reinhard; Klemann, Volker; Bagge, Meike; Ganopolski, Andrey (27 March 2023). "Multistability and Transient Response of the Greenland Ice Sheet to Anthropogenic CO2 Emissions".
592:
Some scientists - including the originators of the hypothesis, Robert DeConto and David Pollard - have suggested that the best way to resolve the question would be to precisely determine sea level rise during the
6370:
Hörhold, M.; Münch, T.; Weißbach, S.; Kipfstuhl, S.; Freitag, J.; Sasgen, I.; Lohmann, G.; Vinther, B.; Laepple, T. (18 January 2023). "Modern temperatures in central–north Greenland warmest in past millennium".
5259:
Xin, Meijiao; Li, Xichen; Stammerjohn, Sharon E; Cai, Wenju; Zhu, Jiang; Turner, John; Clem, Kyle R; Song, Chentao; Wang, Wenzhu; Hou, Yurong (17 May 2023). "A broadscale shift in antarctic temperature trends".
3872:
Dumitru, Oana A.; Dyer, Blake; Austermann, Jacqueline; Sandstrom, Michael R.; Goldstein, Steven L.; D'Andrea, William J.; Cashman, Miranda; Creel, Roger; Bolge, Louise; Raymo, Maureen E. (15 September 2023).
4749:
Hein, Andrew S.; Woodward, John; Marrero, Shasta M.; Dunning, Stuart A.; Steig, Eric J.; Freeman, Stewart P. H. T.; Stuart, Finlay M.; Winter, Kate; Westoby, Matthew J.; Sugden, David E. (3 February 2016).
611: ft). As of 2023, the most recent analysis indicates that the Last Interglacial SLR is unlikely to have been higher than 2.7 m (9 ft), as higher values in other research, such as 5.7 m (
347:
shelves are always stable under mean annual temperatures of −9 °C, but never stable above −5 °C; this places regional warming of 1.5 °C, as preceded the collapse of Larsen B, in context.
255:
On an unrelated hour-to-hour basis, surges of ice motion can be modulated by tidal activity. The influence of a 1 m tidal oscillation can be felt as much as 100 km from the sea. During larger
832:. There has been warming over the ice sheet since the 1950s, and a substantial retreat of its coastal glaciers since at least the 1990s. Estimates suggest it added around 7.6 ± 3.9 mm (
312:
icebergs at their periphery if they experience excess of ice. Ice shelves would also experience accelerated calving due to basal melting. In Antarctica, this is driven by heat fed to the shelf by the
856:
between 1992 and 2017, and has been losing ice in the 2010s at a rate equivalent to 0.4 millimetres (0.016 inches) of annual sea level rise. While some of its losses are offset by the growth of the
7536:
Barr, Iestyn D.; Spagnolo, Matteo; Rea, Brice R.; Bingham, Robert G.; Oien, Rachel P.; Adamson, Kathryn; Ely, Jeremy C.; Mullan, Donal J.; Pellitero, Ramón; Tomkins, Matt D. (21 September 2022).
378:
Even if the ice sheet is grounded below the sea level, MISI cannot occur as long as there is a stable ice shelf in front of it. The boundary between the ice sheet and the ice shelf, known as the
8053:
Koenig, S. J.; Dolan, A. M.; de Boer, B.; Stone, E. J.; Hill, D. J.; DeConto, R. M.; Abe-Ouchi, A.; Lunt, D. J.; Pollard, D.; Quiquet, A.; Saito, F.; Savage, J.; van de Wal, R. (5 March 2015).
6781:
Armstrong McKay, David; Abrams, Jesse; Winkelmann, Ricarda; Sakschewski, Boris; Loriani, Sina; Fetzer, Ingo; Cornell, Sarah; Rockström, Johan; Staal, Arie; Lenton, Timothy (9 September 2022).
5538:
Armstrong McKay, David; Abrams, Jesse; Winkelmann, Ricarda; Sakschewski, Boris; Loriani, Sina; Fetzer, Ingo; Cornell, Sarah; Rockström, Johan; Staal, Arie; Lenton, Timothy (9 September 2022).
3047:
Armstrong McKay, David; Abrams, Jesse; Winkelmann, Ricarda; Sakschewski, Boris; Loriani, Sina; Fetzer, Ingo; Cornell, Sarah; Rockström, Johan; Staal, Arie; Lenton, Timothy (9 September 2022).
1409:
broke apart sending large flotillas of icebergs into the North Atlantic. When these icebergs melted they dropped the boulders and other continental rocks they carried, leaving layers known as
224:
5838:
Noël, B.; van Kampenhout, L.; Lenaerts, J. T. M.; van de Berg, W. J.; van den Broeke, M. R. (19 January 2021). "A 21st Century Warming Threshold for Sustained Greenland Ice Sheet Mass Loss".
585: ft)-tall cliffs), unless the ice had already been substantially damaged beforehand. Further, ice cliff breakdown would produce a large number of debris in the coastal waters - known as
6730:
David P.; Hidy, Alan J.; Perdrial, Nicolas; Peteet, Dorothy M.; Steig, Eric J.; Thomas, Elizabeth K. (20 July 2023). "Deglaciation of northwestern Greenland during Marine Isotope Stage 11".
3230:
Dow, Christine F.; Lee, Won Sang; Greenbaum, Jamin S.; Greene, Chad A.; Blankenship, Donald D.; Poinar, Kristin; Forrest, Alexander L.; Young, Duncan A.; Zappa, Christopher J. (2018-06-01).
7094:
Dieser, Markus; Broemsen, Erik L J E; Cameron, Karen A; King, Gary M; Achberger, Amanda; Choquette, Kyla; Hagedorn, Birgit; Sletten, Ron; Junge, Karen; Christner, Brent C (17 April 2014).
4362:
Li, Qian; England, Matthew H.; Hogg, Andrew McC.; Rintoul, Stephen R.; Morrison, Adele K. (29 March 2023). "Abyssal ocean overturning slowdown and warming driven by Antarctic meltwater".
439:
106:
heat. In places, melting occurs and the melt-water lubricates the ice sheet so that it flows more rapidly. This process produces fast-flowing channels in the ice sheet — these are
6154:
1020:
is typically warmest near the surface and becomes cooler at greater elevation, atmosphere during the Antarctic winter is cooler at the surface than in its middle layers. Consequently,
539:(viewed from the top) would do a lot to determine how quickly it may proceed. Bays which are deep or narrow towards the exit would experience much less rapid retreat than the opposite
1311:
Estimated carbon fluxes are measured in Tg C a (megatonnes of carbon per year) and estimated sizes of carbon stores are measured in Pg C (thousands of megatonnes of carbon). DOC =
4313:
Silvano, Alessandro; Rintoul, Stephen Rich; Peña-Molino, Beatriz; Hobbs, William Richard; van Wijk, Esmee; Aoki, Shigeru; Tamura, Takeshi; Williams, Guy Darvall (18 April 2018).
2930:
Roberts, Jason; Galton-Fenzi, Benjamin K.; Paolo, Fernando S.; Donnelly, Claire; Gwyther, David E.; Padman, Laurie; Young, Duncan; Warner, Roland; Greenbaum, Jamin (2017-08-23).
243:
on a glacier until it begins to flow. The flow velocity and deformation will increase as the equilibrium line between these two processes is approached. This motion is driven by
8016:
Solgaard, Anne M.; Bonow, Johan M.; Langen, Peter L.; Japsen, Peter; Hvidberg, Christine (27 September 2013). "Mountain building and the initiation of the Greenland Ice Sheet".
7479:
Crémière, Antoine; Lepland, Aivo; Chand, Shyam; Sahy, Diana; Condon, Daniel J.; Noble, Stephen R.; Martma, Tõnu; Thorsnes, Terje; Sauer, Simone; Brunstad, Harald (11 May 2016).
6053:
9368:
6639:
Mouginot, Jérémie; Rignot, Eric; Bjørk, Anders A.; van den Broeke, Michiel; Millan, Romain; Morlighem, Mathieu; Noël, Brice; Scheuchl, Bernd; Wood, Michael (20 March 2019).
6423:
de Vernal, Anne; Downs, Jacob; Larour, Eric; Nowicki, Sophie (30 September 2020). "Rate of mass loss from the Greenland Ice Sheet will exceed Holocene values this century".
5484:
King, M. A.; Bingham, R. J.; Moore, P.; Whitehouse, P. L.; Bentley, M. J.; Milne, G. A. (2012). "Lower satellite-gravimetry estimates of Antarctic sea-level contribution".
6867:
410:
Because the entire West Antarctic Ice Sheet is grounded below the sea level, it would be vulnerable to geologically rapid ice loss in this scenario. In particular, the
3770:
Bassis, J. N.; Berg, B.; Crawford, A. J.; Benn, D. I. (18 June 2021). "Transition to marine ice cliff instability controlled by ice thickness gradients and velocity".
669:, with an area of 14 million square kilometres (5.4 million square miles) and an average thickness of over 2 kilometres (1.2 mi). It is the largest of
9544:
1832:
499:
could have occurred - yet more recent research found that these sea level rise episodes can be explained without any ice cliff instability taking place. Research in
200:
crashed in Greenland in 1942. It was only recovered 50 years later. By then, it had been buried under 81 m (268 feet) of ice which had formed over that time period.
6582:
Aschwanden, Andy; Fahnestock, Mark A.; Truffer, Martin; Brinkerhoff, Douglas J.; Hock, Regine; Khroulev, Constantine; Mottram, Ruth; Khan, S. Abbas (19 June 2019).
4625:
Pan, Linda; Powell, Evelyn M.; Latychev, Konstantin; Mitrovica, Jerry X.; Creveling, Jessica R.; Gomez, Natalya; Hoggard, Mark J.; Clark, Peter U. (30 April 2021).
9212:
7757:
Diester-Haass, Liselotte; Zahn, Rainer (1996). "Eocene-Oligocene transition in the Southern Ocean: History of water mass circulation and biological productivity".
996:. The ice sheet is around 2.2 km (1.4 mi) thick on average and is 4,897 m (16,066 ft) at its thickest point. It is also home to the geographic
3677:
Parizek, Byron R.; Christianson, Knut; Alley, Richard B.; Voytenko, Denis; Vaňková, Irena; Dixon, Timothy H.; Walker, Ryan T.; Holland, David M. (22 March 2019).
1797:
Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change
6710:
Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change
6551:
Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change
4300:
Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change
2759:
Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change
1766:
Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change
6517:
319:
The presence of ice shelves has a stabilizing influence on the glacier behind them, while an absence of an ice shelf becomes destabilizing. For instance, when
9385:
6712:
6554:
2584:
6118:
597:. MICI can be effectively ruled out if SLR at the time was lower than 4 m (13 ft), while it is very likely if the SLR was greater than 6 m (
1509:
of 600 ppm, was the primary agent forcing Antarctic glaciation. The glaciation was favored by an interval when the Earth's orbit favored cool summers but
491:
At the same time, this theory has also been highly controversial. It was originally proposed in order to describe how the large sea level rise during the
8821:
8647:
7151:
Znamínko, Matěj; Falteisek, Lukáš; Vrbická, Kristýna; Klímová, Petra; Christiansen, Jesper R.; Jørgensen, Christian J.; Stibal, Marek (16 October 2023).
343:- all started to flow at a much faster rate, while the two glaciers (Flask and Leppard) stabilized by the remnants of the ice shelf did not accelerate.
180:
An ice sheet is a body of ice which covers a land area of continental size - meaning that it exceeds 50,000 km. The currently existing two ice sheets in
984:
longitudinally. It was first formed around 34 million years ago, and it is the largest ice sheet on the entire planet, with far greater volume than the
8816:
5046:
Fretwell, P.; Pritchard, H. D.; Vaughan, D. G.; Bamber, J. L.; Barrand, N. E.; Bell, R.; Bianchi, C.; Bingham, R. G.; Blankenship, D. D. (2013-02-28).
4956:
Fretwell, P.; Pritchard, H. D.; Vaughan, D. G.; Bamber, J. L.; Barrand, N. E.; Bell, R.; Bianchi, C.; Bingham, R. G.; Blankenship, D. D. (2013-02-28).
7320:
6701:
8684:
8018:
4921:"Antarctica and Global Paleogeography: From Rodinia, Through Gondwanaland and Pangea, to the Birth of the Southern Ocean and the Opening of Gateways"
3514:
8621:
6307:
7855:
1235:, the ice sheet is now the warmest it has been in the past 1000 years, and is losing ice at the fastest rate in at least the past 12,000 years.
9706:
7342:
Heinrich, Hartmut (March 1988). "Origin and Consequences of Cyclic Ice Rafting in the Northeast Atlantic Ocean During the Past 130,000 Years".
8330:
6894:
Wadham, J. L.; Hawkings, J. R.; Tarasov, L.; Gregoire, L. J.; Spencer, R. G. M.; Gutjahr, M.; Ridgwell, A.; Kohfeld, K. E. (15 August 2019).
6144:
1711:
1057:
billion tons per year between 2002 and 2010. It is most likely to first see sustained losses of ice at its most vulnerable locations such as
1727:
8563:
3710:
Clerc, Fiona; Minchew, Brent M.; Behn, Mark D. (21 October 2019). "Marine Ice Cliff Instability Mitigated by Slow Removal of Ice Shelves".
1124:
3650:
Olsen, Kira G.; Nettles, Meredith (8 June 2019). "Constraints on Terminus Dynamics at Greenland Glaciers From Small Glacial Earthquakes".
8447:
4724:
4465:
Carlson, Anders E.; Walczak, Maureen H.; Beard, Brian L.; Laffin, Matthew K.; Stoner, Joseph S.; Hatfield, Robert G. (10 December 2018).
3998:
3748:
6231:"A multimillion-year-old record of Greenland vegetation and glacial history preserved in sediment beneath 1.4 km of ice at Camp Century"
5434:"Mass balance of the Antarctic ice sheet 1992–2016: reconciling results from GRACE gravimetry with ICESat, ERS1/2 and Envisat altimetry"
8706:
8664:
1788:
Lemke, P.; Ren, J.; Alley, R.B.; Allison, I.; Carrasco, J.; Flato, G.; Fujii, Y.; Kaser, G.; Mote, P.; Thomas, R.H.; Zhang, T. (2007).
445:
A collage of footage and animation to explain the changes that are occurring on the West Antarctic Ice Sheet, narrated by glaciologist
7603:
4024:
3938:
9585:
8701:
8286:
6078:
Knutz, Paul C.; Newton, Andrew M. W.; Hopper, John R.; Huuse, Mads; Gregersen, Ulrik; Sheldon, Emma; Dybkjær, Karen (15 April 2019).
1027:
Due to these factors, East Antarctica had experienced slight cooling for decades while the rest of the world warmed as the result of
6022:
5354:
8916:
8637:
8355:
8132:
5731:
5696:
5201:
5149:
Scambos, T. A.; Campbell, G. G.; Pope, A.; Haran, T.; Muto, A.; Lazzara, M.; Reijmer, C. H.; Van Den Broeke, M. R. (25 June 2018).
1207:, near its northern edge. The ice sheet covers 1,710,000 square kilometres (660,000 sq mi), around 80% of the surface of
5759:
5663:
2602:
9272:
9061:
8229:
6836:
2035:"Constraints on melt-water flux through the West Greenland ice-sheet: modeling of hydro- fracture drainage of supraglacial lakes"
555:
and stabilized) could have involved MICI, but there weren't enough observations to confirm or refute this theory. The retreat of
272:. Water that reaches the bed of a glacier may freeze there, increasing the thickness of the glacier by pushing it up from below.
79:
that covers surrounding terrain and is greater than 50,000 km (19,000 sq mi). The only current ice sheets are the
10327:
8921:
8884:
8738:
8723:
8642:
8291:
8235:
6961:
Ryu, Jong-Sik; Jacobson, Andrew D. (6 August 2012). "CO2 evasion from the Greenland Ice Sheet: A new carbon-climate feedback".
6331:"Setting a chronology for the basal ice at Dye-3 and GRIP: Implications for the long-term stability of the Greenland Ice Sheet"
5228:"West-warming East-cooling trend over Antarctica reversed since early 21st century driven by large-scale circulation variation"
1454:
877:
7706:
Coxall, Helen K. (2005). "Rapid stepwise onset of Antarctic glaciation and deeper calcite compensation in the Pacific Ocean".
6859:
5599:
4597:
3113:
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7403:
4940:
4100:
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1768:. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp. 2215–2256, doi:10.1017/9781009157896.022.
1250:
goal of staying below 2 °C (3.6 °F) is achieved, melting of Greenland ice alone would still add around 6 cm (
9602:
8558:
8553:
8102:
2400:
2123:
Walker, Dziga P.; Brandon, Mark A.; Jenkins, Adrian; Allen, John T.; Dowdeswell, Julian A.; Evans, Jeff (16 January 2007).
1506:
1309:
Carbon stores and fluxes in present-day ice sheets (2019), and the predicted impact on carbon dioxide (where data exists).
1024:
actually trap heat in the middle atmosphere and reduce its flow towards the surface while the temperature inversion lasts.
1824:
1569:
for most of the past 18 million years, these ice bodies were probably similar to various smaller modern examples, such as
9083:
8861:
8679:
8611:
8601:
8584:
8491:
8298:
5786:
Tan, Ning; Ladant, Jean-Baptiste; Ramstein, Gilles; Dumas, Christophe; Bachem, Paul; Jansen, Eystein (12 November 2018).
4315:"Freshening by glacial meltwater enhances the melting of ice shelves and reduces the formation of Antarctic Bottom Water"
4099:
Dalaiden, Quentin; Schurer, Andrew P.; Kirchmeier-Young, Megan C.; Goosse, Hugues; Hegerl, Gabriele C. (24 August 2022).
860:, Antarctica as a whole will most likely lose enough ice by 2100 to add 11 cm (4.3 in) to sea levels. Further,
8616:
5930:
Bochow, Nils; Poltronieri, Anna; Robinson, Alexander; Montoya, Marisa; Rypdal, Martin; Boers, Niklas (18 October 2023).
896:
of ice-free land may also add around 1 m (3 ft 3 in) to the global sea levels over another 1,000 years.
589:- and multiple studies indicate their build-up would slow or even outright stop the instability soon after it started.
10342:
9699:
9512:
9373:
9330:
8826:
5151:"Ultralow Surface Temperatures in East Antarctica From Satellite Thermal Infrared Mapping: The Coldest Places on Earth"
2623:
Gardner, A. S.; Moholdt, G.; Scambos, T.; Fahnstock, M.; Ligtenberg, S.; van den Broeke, M.; Nilsson, J. (2018-02-13).
1937:
Bindschadler, Robert A.; King, Matt A.; Alley, Richard B.; Anandakrishnan, Sridhar; Padman, Laurence (22 August 2003).
488:. Sea level rise projections which involve MICI are much larger than the others, particularly under high warming rate.
17:
7039:"First observation of direct methane emission to the atmosphere from the subglacial domain of the Greenland Ice Sheet"
6719:. Cambridge University Press, Cambridge, United Kingdom and New York, NY, US, pp. 3–32, doi:10.1017/9781009157896.001.
9439:
9315:
9132:
8335:
6302:
5205:
1354:. Also for comparison, the annual human caused carbon dioxide emissions amount to around 40 billion tonnes of CO
1327:
and were largely disregarded in global models. In 2010s, research had demonstrated the existence of uniquely adapted
1279: in) since 1972, while sea level rise from all sources was 15–25 cm (6–10 in)) between 1901 and 2018.
1246:
the ice sheet is melting two to five times faster than before 1850, and snowfall has not kept up since 1996. If the
883:
In the long term, the West Antarctic Ice Sheet is likely to disappear due to the warming which has already occurred.
6507:
3179:
DeConto, Robert M.; Pollard, David (30 March 2016). "Contribution of Antarctica to past and future sea-level rise".
2034:
1405:
For instance, during at least the last 100,000 years, portions of the ice sheet covering much of North America, the
192:
This process of ice sheet growth is still occurring nowadays, as can be clearly seen in an example that occurred in
9672:
9310:
9290:
9237:
9189:
8251:
5226:
Xin, Meijiao; Clem, Kyle R; Turner, John; Stammerjohn, Sharon E; Zhu, Jiang; Cai, Wenju; Li, Xichen (2 June 2023).
1603:, formed a lower planation surface at 500 to 1000 meters above sea level. A third stage of uplift created multiple
1335:
and physical weathering in ice sheets, and storage and cycling of organic carbon in excess of 100 billion tonnes.
1032:
673:, containing 26.5 million cubic kilometres (6,400,000 cubic miles) of ice, which is equivalent to 61% of all
9429:
9380:
8806:
8768:
8713:
8183:
7096:"Molecular and biogeochemical evidence for methane cycling beneath the western margin of the Greenland Ice Sheet"
6543:
4292:
2751:
1440:
has been observed by linking short-term spikes of methane in Greenland ice cores and Antarctic ice cores. During
1040:
7778:
6079:
2881:
Greene, Chad A.; Young, Duncan A.; Gwyther, David E.; Galton-Fenzi, Benjamin K.; Blankenship, Donald D. (2018).
2527:
1761:
9497:
8781:
8538:
7610:
Palaeogeography, palaeoclimatology, & palaeoecology ISSN 0031-0182, 1992, vol. 93, no1-2, pp. 85–112 (3 p.)
3583:"Stabilizing effect of mélange buttressing on the marine ice-cliff instability of the West Antarctic Ice Sheet"
2982:
Greene, Chad A.; Blankenship, Donald D.; Gwyther, David E.; Silvano, Alessandro; Wijk, Esmee van (2017-11-01).
2834:"Mass Loss of Totten and Moscow University Glaciers, East Antarctica, Using Regionally Optimized GRACE Mascons"
1011:
The surface of the EAIS is the driest, windiest, and coldest place on Earth. Lack of moisture in the air, high
235:
to an imbalance between high ice accumulation in the central plateau and lower accumulation, as well as higher
8097:
1795:. In Solomon, S.; Qin, D.; Manning, M.; Chen, Z.; Marquis, M.; Averyt, K.B.; Tignor, M.; Miller, H.L. (eds.).
677:
on Earth. Its surface is nearly continuous, and the only ice-free areas on the continent are the dry valleys,
9692:
9607:
9142:
8674:
7645:
Pagani, M.; Huber, M.; Liu, Z.; Bohaty, S. M.; Henderiks, J.; Sijp, W.; Krishnan, S.; Deconto, R. M. (2011).
4136:
1546:
682:
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8786:
8691:
8568:
8125:
6698:
6149:
5288:
1441:
1430:
1332:
1117:
861:
485:
5432:
Zwally, H. Jay; Robbins, John W.; Luthcke, Scott B.; Loomis, Bryant D.; Rémy, Frédérique (29 March 2021).
3875:"Last interglacial global mean sea level from high-precision U-series ages of Bahamian fossil coral reefs"
3561:
1049:
Because the East Antarctic ice sheet has barely warmed, it is still gaining ice on average. for instance,
8801:
8654:
3146:
1594:
1362:
7481:"Timescales of methane seepage on the Norwegian margin following collapse of the Scandinavian Ice Sheet"
1810:
1789:
9825:
9660:
9424:
9227:
9184:
8957:
8879:
8733:
5375:
Steig, E. J.; Schneider, D. P.; Rutherford, S. D.; Mann, M. E.; Comiso, J. C.; Shindell, D. T. (2009).
4627:"Rapid postglacial rebound amplifies global sea level rise following West Antarctic Ice Sheet collapse"
4042:
Steig, E. J.; Schneider, D. P.; Rutherford, S. D.; Mann, M. E.; Comiso, J. C.; Shindell, D. T. (2009).
3619:"Evaluating the Retreat, Arrest, and Regrowth of Crane Glacier Against Marine Ice Cliff Process Models"
1510:
1316:
6297:
4807:
Garbe, Julius; Albrecht, Torsten; Levermann, Anders; Donges, Jonathan F.; Winkelmann, Ricarda (2020).
4598:"Exceeding 1.5 °C global warming could trigger multiple climate tipping points – paper explainer"
3151:. The International Conference on Materials Chemistry and Environmental Engineering (CONF-MCEE 2021).
1305:
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9204:
9179:
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8696:
8659:
8409:
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7620:
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3471:
1505:
and had been decreasing from earlier levels in the thousands of ppm. Carbon dioxide decrease, with a
406:, the location of both Thwaites (TEIS refers to Thwaites Eastern Ice Shelf) and Pine Island Glaciers.
9044:
9539:
9534:
9524:
9465:
9305:
8811:
8776:
8669:
8596:
8437:
8266:
8202:
8163:
7601:
Sedimentological evidence for the formation of an East Antarctic ice sheet in Eocene/Oligocene time
4101:"West Antarctic Surface Climate Changes Since the Mid-20th Century Driven by Anthropogenic Forcing"
1612:
1370:
1344:
1312:
1232:
993:
989:
973:
965:
857:
798:
782:
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694:
690:
368:
189:
falls onto the ice sheet never melts, and is instead compressed by the mass of newer snow layers.
7210:"A mechanism for reconciling the synchronisation of Heinrich events and Dansgaard-Oeschger cycles"
5788:"Dynamic Greenland ice sheet driven by pCO2 variations across the Pliocene Pleistocene transition"
2475:
Mercer, J. H. (1978). "West Antarctic ice sheet and CO2 greenhouse effect: a threat of disaster".
2420:"Ocean variability beneath Thwaites Eastern Ice Shelf driven by the Pine Island Bay Gyre strength"
2175:"Glacier acceleration and thinning after ice shelf collapse in the Larsen B embayment, Antarctica"
1708:
9648:
9570:
9480:
9222:
9194:
8874:
8533:
8511:
8118:
7646:
5293:
1731:
1627:
2.7–2.6 million years ago, by which time temperatures had dropped sufficiently for the disparate
1340:
568:
6860:"Exceeding 1.5°C global warming could trigger multiple climate tipping points – paper explainer"
5600:"Exceeding 1.5°C global warming could trigger multiple climate tipping points – paper explainer"
3114:"Exceeding 1.5°C global warming could trigger multiple climate tipping points – paper explainer"
1513:
marker changes were too large to be explained by Antarctic ice-sheet growth alone indicating an
10317:
9247:
9067:
9009:
8926:
8911:
8796:
8442:
8388:
8383:
8378:
8373:
8368:
8363:
6996:
Tarnocai, C.; Canadell, J.G.; Schuur, E.A.G.; Kuhry, P.; Mazhitova, G.; Zimov, S. (June 2009).
4920:
4418:"Unavoidable future increase in West Antarctic ice-shelf melting over the twenty-first century"
873:
313:
4466:
3513:
Wise, Matthew G.; Dowdeswell, Julian A.; Jakobsson, Martin; Larter, Robert D. (October 2017).
1535:
opened up. But there was no significant decline in the land-based Eastern Antarctic ice sheet.
9728:
9636:
9282:
9159:
8967:
8427:
8350:
7208:
Schannwell, Clemens; Mikolajewicz, Uwe; Kapsch, Marie-Luise; Ziemen, Florian (5 April 2024).
4808:
4683:
3957:
1653:
1328:
1216:
1036:
516:
6346:
6041:
4208:
The IMBIE Team (13 June 2018). "Mass balance of the Antarctic Ice Sheet from 1992 to 2017".
3515:"Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks"
2302:
1099:
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10131:
9475:
9353:
9014:
8589:
8516:
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7924:
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7433:
7351:
7270:
7164:
7107:
7050:
7009:
6970:
6907:
6739:
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6037:
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4057:
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3529:
3450:
3365:
3305:
3243:
3188:
2995:
2946:
2894:
2845:
2782:
2685:
2636:
2625:"Increased West Antarctic and unchanged East Antarctic ice discharge over the last 7 years"
2542:
2484:
2431:
2347:
2298:
2186:
2139:
2081:
2042:
1997:
1920:
1908:
1853:
Easterbrook, Don J., Surface Processes and Landforms, 2nd Edition, Prentice-Hall Inc., 1999
1695:
1665:
1406:
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710:
300:
As the margins end at the marine boundary, excess ice is discharged through ice streams or
154:
138:
134:
7153:"Methylotrophic Communities Associated with a Greenland Ice Sheet Methane Release Hotspot"
5377:"Warming of the Antarctic ice-sheet surface since the 1957 International Geophysical Year"
5344:
4044:"Warming of the Antarctic ice-sheet surface since the 1957 International Geophysical Year"
3581:
Schlemm, Tanja; Feldmann, Johannes; Winkelmann, Ricarda; Levermann, Anders (24 May 2022).
3350:
3161:
8:
10347:
10337:
10322:
10020:
9853:
9492:
9267:
8501:
8496:
6080:"Eleven phases of Greenland Ice Sheet shelf-edge advance over the past 2.7 million years"
4752:"Evidence for the stability of the West Antarctic Ice Sheet divide for 1.4 million years"
1395:
1324:
1242:
into the sea. Normally the ice sheet would be replenished by winter snowfall, but due to
1212:
1204:
1199:
1191:
1001:
985:
981:
908:
904:
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655:
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512:
415:
324:
185:
181:
173:
130:
103:
84:
80:
42:
31:
8070:
8031:
7991:
7928:
7913:"Minimal East Antarctic Ice Sheet retreat onto land during the past eight million years"
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7816:
7770:
7719:
7662:
7553:
7496:
7437:
7355:
7274:
7234:
7209:
7185:
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7152:
7111:
7054:
7013:
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6911:
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6656:
6599:
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5931:
5851:
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5688:
5497:
5394:
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4879:
4824:
4767:
4702:
4642:
4496:
4433:
4375:
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4176:
4119:
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3783:
3533:
3454:
3369:
3309:
3247:
3192:
2999:
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2898:
2849:
2786:
2689:
2640:
2546:
2488:
2435:
2351:
2190:
2143:
2085:
2046:
2001:
1912:
864:
may increase this amount by tens of centimeters, particularly under high warming. Fresh
10332:
9320:
9252:
9169:
9019:
8984:
8941:
8936:
8931:
8506:
7956:
7893:
7836:
7739:
7682:
7513:
7480:
7456:
7422:"Early Last Interglacial ocean warming drove substantial ice mass loss from Antarctica"
7421:
7367:
7286:
7128:
7095:
7071:
7038:
6938:
6895:
6828:
6763:
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5907:
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4863:
4844:
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4751:
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4578:
4516:
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4339:
4314:
4251:
4190:
4141:
4081:
3990:
3492:
3331:
3272:
3231:
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3094:
3024:
2983:
2931:
2863:
2814:
2725:
2566:
2508:
2452:
2419:
2376:
2335:
2287:"Potential Antarctic Ice Sheet retreat driven by hydrofracturing and ice cliff failure"
2214:
2155:
2125:"Oceanic heat transport onto the Amundsen Sea shelf through a submarine glacial trough"
2124:
2105:
2015:
1966:
1050:
977:
802:
560:
7793:
6782:
5539:
3048:
1986:"Ice stream D flow speed is strongly modulated by the tide beneath the Ross Ice Shelf"
1593:, and ultimately formed the upper planation surface at a height of 2000 to 3000 meter
10215:
10171:
10121:
10030:
9995:
9554:
9217:
8962:
8728:
8521:
8484:
8271:
8225:
8055:"Ice sheet model dependency of the simulated Greenland Ice Sheet in the mid-Pliocene"
7948:
7940:
7885:
7828:
7731:
7686:
7674:
7583:
7575:
7537:
7518:
7461:
7399:
7371:
7363:
7294:
7239:
7190:
7133:
7076:
6943:
6832:
6820:
6812:
6767:
6755:
6680:
6621:
6475:"Special Report on the Ocean and Cryosphere in a Changing Climate: Executive Summary"
6460:
6448:
6396:
6278:
6260:
6202:
6114:
6023:"Modelling Greenland ice sheet inception and sustainability during the Late Pliocene"
5969:
5911:
5875:
5817:
5581:
5569:
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5406:
5135:
5087:
4997:
4936:
4901:
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4836:
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4570:
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4387:
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4243:
4194:
4145:
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2709:
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2500:
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2258:
2097:
1958:
1879:
1624:
1578:
1570:
1502:
1422:
1410:
917:
893:
805:. It is classified as a marine-based ice sheet, meaning that its bed lies well below
594:
496:
387:
356:
265:
119:
37:
7999:
7960:
7897:
4720:
4255:
3994:
3891:
3874:
3496:
2729:
2218:
2159:
2109:
2019:
1970:
911:
to preserve them. In theory, adding thousands of gigatonnes of artificially created
10250:
10146:
10015:
9947:
9597:
9164:
9147:
9088:
8979:
8743:
8467:
8340:
8276:
8074:
8035:
7995:
7932:
7877:
7860:
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7820:
7774:
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7666:
7565:
7557:
7508:
7500:
7451:
7441:
7391:
7359:
7278:
7229:
7221:
7180:
7172:
7123:
7115:
7066:
7058:
7017:
6978:
6933:
6923:
6915:
6802:
6794:
6747:
6670:
6660:
6611:
6603:
6440:
6408:
6388:
6350:
6268:
6250:
6214:
6194:
6102:
6045:
6000:
5959:
5951:
5899:
5863:
5855:
5807:
5799:
5634:
5593:
5591:
5559:
5551:
5521:
5501:
5445:
5418:
5398:
5381:
5269:
5239:
5180:
5170:
5121:
5077:
5067:
5025:
4987:
4977:
4928:
4891:
4883:
4828:
4779:
4771:
4706:
4654:
4646:
4552:
4544:
4500:
4437:
4379:
4334:
4326:
4302:. Cambridge University Press, Cambridge, UK and New York, New York, USA: 1270–1272.
4233:
4225:
4180:
4131:
4123:
4085:
4065:
4048:
3980:
3916:
3886:
3849:
3841:
3795:
3787:
3727:
3719:
3690:
3659:
3630:
3594:
3537:
3466:
3458:
3420:
3412:
3373:
3321:
3313:
3267:
3251:
3196:
3156:
3068:
3060:
3019:
3003:
2954:
2902:
2853:
2818:
2790:
2701:
2693:
2644:
2550:
2512:
2492:
2447:
2439:
2371:
2355:
2306:
2248:
2204:
2194:
2147:
2089:
2005:
1950:
1916:
1871:
1418:
900:
508:
411:
336:
7743:
6982:
6329:
Yau, Audrey M.; Bender, Michael L.; Blunier, Thomas; Jouzel, Jean (15 July 2016).
2418:
Dotto, Tiago S.; Heywood, Karen J.; Hall, Rob A.; et al. (21 December 2022).
1611:
below the planation surfaces. This uplift intensified glaciation due to increased
1394:
Normally, the transitions between glacial and interglacial states are governed by
1385:
304:. Then, it either falls directly into the sea or is accumulated atop the floating
122:. These lakes may feed warm water to glacial bases and facilitate glacial motion.
102:
Although the surface is cold, the base of an ice sheet is generally warmer due to
10220:
10141:
10126:
10080:
10060:
9747:
9549:
9470:
9434:
9363:
9337:
9325:
9242:
9174:
9049:
8906:
8528:
8479:
8457:
8039:
7607:
7282:
6995:
6716:
6705:
6474:
3232:"Basal channels drive active surface hydrology and transverse ice shelf fracture"
1715:
1671:
1620:
1414:
1247:
1066:
1044:
814:
790:
564:
504:
500:
403:
269:
150:
6851:
5588:
5289:"Media goofed on Antarctic data / Global warming interpretation irks scientists"
1521:
may have played a role as well though models of the changes suggest declining CO
249:
10065:
9762:
9502:
9358:
9300:
9295:
9137:
9026:
8758:
8753:
8748:
8606:
8543:
8281:
8261:
8220:
8141:
7561:
7225:
7176:
7062:
6919:
6584:"Contribution of the Greenland Ice Sheet to sea level over the next millennium"
6355:
6330:
6049:
5955:
5803:
5273:
5244:
5227:
5126:
5110:"Low Antarctic continental climate sensitivity due to high ice sheet orography"
5109:
4442:
4417:
4383:
4185:
4161:"Evidence for rapid retreat and mass loss of Thwaites Glacier, West Antarctica"
4160:
3845:
2443:
2359:
2311:
2286:
2050:
1659:
1586:
1265:
1243:
1058:
1028:
1021:
853:
829:
810:
525:
423:
327:
had collapsed over three weeks in February 2002, the four glaciers behind it -
301:
213:
126:
7936:
6783:"Exceeding 1.5°C global warming could trigger multiple climate tipping points"
6444:
6106:
6021:
Contoux, C.; Dumas, C.; Ramstein, G.; Jost, A.; Dolan, A.M. (15 August 2015).
5540:"Exceeding 1.5°C global warming could trigger multiple climate tipping points"
5533:
5531:
4832:
4229:
3462:
3317:
3049:"Exceeding 1.5°C global warming could trigger multiple climate tipping points"
2697:
2554:
2284:
2253:
2236:
1875:
1350:
For comparison, 1400–1650 billion tonnes are contained within the Arctic
586:
531:
30:"Continental glacier" redirects here. For the glacier located in Wyoming, see
10311:
10151:
9985:
9684:
9575:
9507:
9232:
9054:
9039:
8974:
8869:
7579:
6816:
6539:
6264:
5573:
5091:
5001:
4566:
4288:
4282:
4280:
3809:
3549:
3480:
3263:
3082:
3015:
2968:
2916:
2802:
2761:. Cambridge University Press, Cambridge, UK and New York, NY, USA: 1270–1272.
2747:
2713:
2658:
2562:
2504:
2367:
2262:
1574:
1518:
1139:
1126:
544:
520:
340:
332:
328:
158:
142:
7794:"Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO
7670:
7446:
6798:
6751:
6665:
6255:
6004:
5555:
5315:
4548:
4504:
3791:
3599:
3582:
3064:
2907:
2882:
2833:
2673:
2093:
2033:
Krawczynski, M. J.; Behn, M. D.; Das, S. B.; Joughin, I. (1 December 2007).
1954:
731:
99:. An ice cap will typically feed a series of glaciers around its periphery.
10136:
9833:
9460:
9257:
8901:
8891:
8548:
8432:
8345:
8079:
8054:
7952:
7889:
7832:
7735:
7678:
7587:
7522:
7465:
7298:
7243:
7194:
7137:
7080:
7037:
Christiansen, Jesper Riis; Jørgensen, Christian Juncher (9 November 2018).
6947:
6824:
6759:
6684:
6625:
6607:
6512:
6452:
6400:
6282:
6206:
5973:
5821:
5638:
5528:
5513:
5410:
5368:
5319:
5029:
4905:
4887:
4840:
4793:
4668:
4650:
4574:
4527:
4512:
4391:
4348:
4330:
4247:
4077:
3920:
3817:
3557:
3488:
3281:
3255:
3208:
3090:
3033:
3007:
2810:
2721:
2649:
2624:
2461:
2385:
2331:
2101:
1962:
1531:
epoch, approximately five to three million years ago; during this time the
1374:
1062:
957:~2.2 km (1.4 mi) (average), ~4.9 km (3.0 mi) (maximum)
884:
822:
626:
398:
240:
197:
193:
169:
7119:
6780:
5537:
5193:
5072:
5048:"Bedmap2: improved ice bed, surface and thickness datasets for Antarctica"
5047:
4982:
4958:"Bedmap2: improved ice bed, surface and thickness datasets for Antarctica"
4957:
4711:
4684:"Bedmap2: improved ice bed, surface and thickness datasets for Antarctica"
4533:
4277:
3985:
3958:"Bedmap2: improved ice bed, surface and thickness datasets for Antarctica"
3046:
1984:
Anandakrishnan, S.; Voigt, D. E.; Alley, R. B.; King, M. A. (April 2003).
1553:
1183:
1.67 km (1.0 mi) (average), ~3.5 km (2.2 mi) (maximum)
758:~1.05 km (0.7 mi) (average), ~2 km (1.2 mi) (maximum)
9915:
9910:
9873:
9487:
9004:
8996:
8256:
7321:"Why Milankovitch (Orbital) Cycles Can't Explain Earth's Current Warming"
7022:
6998:"Soil organic carbon pools in the northern circumpolar permafrost region"
6997:
5903:
5859:
5175:
5150:
4127:
3723:
3663:
3635:
3618:
3425:
3416:
3377:
2883:"Seasonal dynamics of Totten Ice Shelf controlled by sea ice buttressing"
2858:
2199:
2174:
2151:
2010:
1985:
1239:
809:
and its edges flow into floating ice shelves. The WAIS is bounded by the
674:
630:
446:
309:
257:
146:
7881:
7824:
7727:
7504:
6807:
6392:
6198:
5564:
5505:
5402:
5041:
5039:
4862:
Feldmann, Johannes; Levermann, Anders; Mengel, Matthias (17 July 2019).
4775:
4557:
4416:
Naughten, Kaitlin A.; Holland, Paul R.; De Rydt, Jan (23 October 2023).
4411:
4409:
4069:
3541:
3351:"Rethinking Sea-Level Projections Using Families and Timing Differences"
3326:
3200:
3073:
2794:
1527:
The Western Antarctic ice sheet declined somewhat during the warm early
1461:
1047:
resulted in consistent net warming across the continent since the 1957.
828:
As a smaller part of Antarctica, WAIS is also more strongly affected by
288:
ice shelf had profound effects on the velocities of its feeder glaciers.
10116:
10035:
9863:
9519:
8896:
7395:
7290:
7258:
6774:
6641:"Forty-six years of Greenland Ice Sheet mass balance from 1972 to 2018"
5867:
5450:
5433:
5280:
5185:
4468:
Absence of the West Antarctic ice sheet during the last interglaciation
4238:
3854:
3800:
2705:
2209:
1647:
1641:
1616:
1557:
Timeline of the ice sheet's formation from 2.9 to 2.6 million years ago
1470:
1399:
1351:
1343:
if it is gradually released through meltwater, thus increasing overall
1017:
997:
794:
702:
663:
107:
61:
46:
7944:
7912:
7570:
6709:
6581:
6577:
6575:
6531:
5082:
4992:
3732:
1765:
1215:. The term 'Greenland ice sheet' is often shortened to GIS or GrIS in
10270:
10161:
10111:
10070:
9980:
9937:
9779:
8474:
8098:
United Nations Environment Programme: Global Outlook for Ice and Snow
5837:
5103:
5101:
5036:
5008:
4864:"Stabilizing the West Antarctic Ice Sheet by surface mass deposition"
4855:
4675:
4406:
4098:
4092:
3695:
3678:
2528:"West Antarctic Ice Sheet collapse – the fall and rise of a paradigm"
2496:
1566:
1478:
1208:
865:
806:
666:
536:
364:
305:
88:
49:
8011:
8009:
5142:
4458:
4306:
2959:
1938:
422:
The majority of the East Antarctic Ice Sheet would not be affected.
292:
280:
10230:
10194:
10184:
10075:
9757:
9719:
7647:"Drop in carbon dioxide levels led to polar ice sheet, study finds"
6572:
6537:
6016:
6014:
5727:
5692:
5425:
5376:
4932:
4620:
4618:
4286:
4152:
4043:
4016:
2745:
1936:
1600:
1532:
1528:
1466:
1282:(2.7 °F) would still cause ice loss equivalent to 1.4 m (
706:
678:
548:
492:
360:
320:
285:
236:
9955:
7972:
7970:
7207:
6691:
6553:. Cambridge University Press, Cambridge, UK and New York, NY, US.
5985:
5983:
5925:
5923:
5921:
5470:
5098:
4800:
4589:
4270:
4201:
4035:
3580:
1589:
which now form the uplands of West and East Greenland experienced
10156:
10096:
10050:
10040:
9975:
9885:
9769:
8452:
8110:
8006:
6638:
6632:
6289:
5932:"Overshooting the critical threshold for the Greenland ice sheet"
5477:
5462:
5336:
5307:
5252:
5219:
4742:
4262:
1939:"Tidally Controlled Stick-Slip Discharge of a West Antarctic Ice"
1628:
1590:
1582:
1562:
1539:
1514:
1482:
1447:
1366:
1227:
1223:
818:
686:
244:
96:
92:
73:
7856:"Obliquity-paced Pliocene West Antarctic ice sheet oscillations"
7538:"60 million years of glaciation in the Transantarctic Mountains"
6363:
6227:
6145:"Scientists chart history of Greenland Ice Sheet for first time"
6136:
6011:
5929:
5617:
4615:
4475:
3676:
2929:
2585:"After Decades of Losing Ice, Antarctica Is Now Hemorrhaging It"
1662: – Worldwide glaciation episodes during the Proterozoic eon
1489:
The icing of Antarctica began in the Late Palaeocene or middle
1373:
than carbon dioxide. However, it also harbours large numbers of
1323:
Historically, ice sheets were viewed as inert components of the
95:. Masses of ice covering less than 50,000 km are termed an
56:
on Earth. It has an average thickness of over 2 kilometers.
10280:
10265:
10260:
10225:
10199:
10179:
10101:
10055:
10045:
9960:
9932:
9922:
9900:
9843:
9815:
9810:
9784:
9455:
7967:
7390:. Geophysical Monograph Series. Vol. 112. pp. 35–58.
7150:
6722:
6467:
6415:
6221:
5980:
5918:
5882:
5833:
5831:
4355:
2981:
1604:
1493:
between 60 and 45.5 million years ago and escalated during the
1490:
1474:
1012:
888:
7621:"New CO2 data helps unlock the secrets of Antarctic formation"
6728:
6169:
6071:
5781:
5779:
5777:
5718:
5716:
5714:
5045:
4955:
4312:
3871:
2880:
2622:
1656: – Series of alternating glacial and interglacial periods
1425:, and occur during cold periods within the last interglacial.
10255:
10245:
10235:
10106:
10025:
10005:
9970:
9965:
9927:
9905:
9890:
9880:
9858:
9838:
9805:
9774:
9742:
9715:
9369:
Cooperative Mechanisms under Article 6 of the Paris Agreement
8462:
7388:
Mechanisms of Global Climate Change at Millennial Time Scales
6893:
6369:
3749:"Collapse may not always be inevitable for marine ice cliffs"
3512:
3349:
Slangen, A. B. A.; Haasnoot, M.; Winter, G. (30 March 2022).
1608:
938:
552:
6322:
5828:
5374:
4806:
4041:
2237:"Stability of the Junction of an Ice Sheet and an Ice Shelf"
2070:
1983:
1365:, where meltwater carbon is released into the atmosphere as
887:
evidence suggests that this has already happened during the
10275:
10189:
9895:
9868:
9848:
9752:
7779:
10.1130/0091-7613(1996)024<0163:EOTITS>2.3.CO;2
7259:"Climate Control: How Large a Role for Orbital Variations?"
6499:
6479:
5774:
5711:
5014:
3905:
3439:
2674:"Mass balance of the Antarctic Ice Sheet from 1992 to 2017"
2285:
David Pollard; Robert M. DeConto; Richard B. Alley (2015).
1455:
Antarctic ice sheet § Situation during geologic time scales
912:
402:
Distribution of meltwater hotspots caused by ice losses in
316:
current, which is 3 °C above the ice's melting point.
7418:
6421:
5623:
5483:
5431:
4748:
4624:
10240:
10010:
9545:
Illustrative model of greenhouse effect on climate change
8015:
7093:
6175:
5989:
5888:
5746:
4464:
2122:
2032:
383:
76:
53:
7478:
6020:
5225:
5148:
5108:
Singh, Hansi A.; Polvani, Lorenzo M. (10 January 2020).
2771:
1709:
American Meteorological Society, Glossary of Meteorology
296:
Accelerated ice flows after the break-up of an ice shelf
8052:
7976:
6508:"Guest post: How the Greenland ice sheet fared in 2022"
5313:
4861:
2417:
670:
456:(MICI) posits that ice cliffs which exceed ~90 m (
363:
is denser than ice, then any ice sheets grounded below
7535:
7384:
6328:
6077:
5785:
5202:"New study explains Antarctica's coldest temperatures"
4481:
4415:
3830:
3769:
3401:
3148:
Reviewing the elements of marine ice cliff instability
2932:"Ocean forced variability of Totten Glacier mass loss"
1813:. National Snow and Ice Data Center. 21 November 2012.
1790:"Observations: Changes in Snow, Ice and Frozen Ground"
470: ft) in above-ground height and are ~800 m (
9386:
United Nations Framework Convention on Climate Change
7036:
3348:
3229:
2336:"The paradigm shift in Antarctic ice sheet modelling"
7644:
6506:
Stendel, Martin; Mottram, Ruth (22 September 2022).
6229:
J.; Caffee, Marc W.; Southon, John (30 March 2021).
4918:
4361:
2984:"Wind causes Totten Ice Shelf melt and acceleration"
2741:
2739:
1865:
1787:
382:, is particularly stable if it is constrained in an
6544:"Chapter 9: Ocean, Cryosphere and Sea Level Change"
5258:
4919:Torsvik, T. H.; Gaina, C.; Redfield, T. F. (2008).
4293:"Chapter 9: Ocean, Cryosphere and Sea Level Change"
3294:
2752:"Chapter 9: Ocean, Cryosphere and Sea Level Change"
1932:
1930:
1756:
1754:
1752:
1750:
1748:
3040:
1977:
1861:
1859:
1465:Polar climatic temperature changes throughout the
633:and the known history of the Greenland Ice Sheet.
367:inherently become less stable as they melt due to
8019:Palaeogeography, Palaeoclimatology, Palaeoecology
7756:
7030:
4137:20.500.11820/64ecd5a1-af19-43e8-9d34-da7274cc4ae0
2736:
1899:Clarke, G. K. C. (2005). "Subglacial processes".
636:
10309:
9586:Intergovernmental Panel on Climate Change (IPCC)
6298:"How and when did the Greenland Ice Sheet form?"
5724:"How Greenland would look without its ice sheet"
5689:"How Greenland would look without its ice sheet"
3709:
2939:Geological Society, London, Special Publications
1927:
1898:
1745:
1728:"Glossary of Important Terms in Glacial Geology"
535:If MICI can occur, the structure of the glacier
7426:Proceedings of the National Academy of Sciences
7201:
6896:"Ice sheets matter for the global carbon cycle"
6857:
6645:Proceedings of the National Academy of Sciences
6235:Proceedings of the National Academy of Sciences
5597:
4595:
3616:
3111:
2618:
2616:
2230:
2228:
2026:
1856:
750:<1,970,000 km (760,000 sq mi)
430:
350:
239:, at the margins. This imbalance increases the
9714:
6889:
6887:
6885:
6505:
4682:Fretwell, P.; et al. (28 February 2013).
4207:
3956:Fretwell, P.; et al. (28 February 2013).
3867:
3865:
3679:"Ice-cliff failure via retrogressive slumping"
3652:Journal of Geophysical Research: Earth Surface
3612:
3610:
3576:
3574:
3405:Journal of Geophysical Research: Earth Surface
3397:
3395:
3393:
3391:
3389:
3387:
3178:
3174:
3172:
2398:
2326:
2324:
2322:
2280:
2278:
2276:
2274:
2272:
1690:
1688:
1540:Greenland ice sheet during geologic timescales
1448:Antarctic ice sheet during geologic timescales
9700:
8331:History of climate change policy and politics
8126:
5457:and Giovinetto (Zwally and Giovinetto, 2011).
3932:
3930:
3617:Needell, C.; Holschuh, N. (20 January 2023).
3155:. Vol. 2152. California, United States.
1901:Annual Review of Earth and Planetary Sciences
1644: – Earth's surface where water is frozen
217:Glacial flow rate in the Antarctic ice sheet.
5107:
4949:
3949:
3649:
3140:
3138:
3136:
3134:
2613:
2401:"Marine Ice Sheet Instability "For Dummies""
2225:
1438:Hemispheric asynchrony in ice sheet behavior
1238:Every summer, parts of the surface melt and
1053:data indicated East Antarctica mass gain of
625: ft), appear inconsistent with the new
8448:Atlantic meridional overturning circulation
6960:
6882:
6858:Armstrong McKay, David (9 September 2022).
5598:Armstrong McKay, David (9 September 2022).
5342:
4912:
4809:"The hysteresis of the Antarctic Ice Sheet"
4596:Armstrong McKay, David (9 September 2022).
3862:
3607:
3571:
3508:
3506:
3384:
3342:
3169:
3112:Armstrong McKay, David (9 September 2022).
2319:
2269:
2166:
1685:
1159:1,710,000 km (660,000 sq mi)
1039:. After 2009, improvements in Antarctica's
924:
717:
543:In recent years, 2002-2004 fast retreat of
9707:
9693:
9667:
9655:
9112:
8133:
8119:
8103:Marine Ice Sheet Instability "For Dummies"
5683:
5681:
4925:Antarctica: A Keystone in a Changing World
4471:. American Geophysical Union Fall Meeting.
3927:
3288:
2831:
2671:
2116:
1892:
1847:
1361:In Greenland, there is one known area, at
992:(WAIS), from which it is separated by the
916:it would still require one of the largest
129:) there were other ice sheets. During the
9407:
9213:Adaptation strategies on the German coast
8356:United Nations Climate Change conferences
8078:
7569:
7512:
7455:
7445:
7233:
7184:
7127:
7070:
7021:
6937:
6929:1983/19a3bd0c-eff6-48f5-a8b0-1908c2404a24
6927:
6806:
6674:
6664:
6615:
6354:
6272:
6254:
5963:
5811:
5563:
5449:
5243:
5184:
5174:
5125:
5081:
5071:
4991:
4981:
4895:
4783:
4710:
4658:
4556:
4441:
4338:
4237:
4184:
4135:
3984:
3890:
3853:
3799:
3731:
3694:
3634:
3598:
3472:1983/de5e9847-612f-42fb-97b0-5d7ff43d37b8
3470:
3424:
3325:
3271:
3160:
3131:
3105:
3072:
3023:
2958:
2906:
2857:
2648:
2451:
2411:
2375:
2310:
2252:
2208:
2198:
2009:
1380:
1035:and occasionally used as an argument for
8917:Co-benefits of climate change mitigation
7341:
6142:
5652:
5650:
5648:
5314:Eric Steig; Gavin Schmidt (2004-12-03).
5286:
5199:
4681:
3955:
3503:
2234:
2064:
1782:
1780:
1778:
1776:
1774:
1668: – North American glacial ice sheet
1631:to connect and cover most of the island.
1552:
1547:Greenland ice sheet § Geological history
1460:
1384:
1304:
530:
434:
397:
291:
279:
220:
212:
168:
36:
9273:National Adaptation Programme of Action
9062:Land use, land-use change, and forestry
7911:Shakun, Jeremy D.; et al. (2018).
7791:
6295:
5678:
3746:
2525:
2172:
1377:bacteria, which limit those emissions.
1300:
689:. However, it is often subdivided into
551:ice shelf (before it reached a shallow
393:
14:
10310:
8922:Economics of climate change mitigation
8885:Gold Standard (carbon offset standard)
8408:
8236:Scientific consensus on climate change
7910:
7705:
4158:
4022:
3936:
2474:
2330:
1921:10.1146/annurev.earth.33.092203.122621
1674: – Simulation of ice sheet change
1623:levels dropped to between 280 and 320
1074:
878:Southern Ocean overturning circulation
701:(AP), due to the large differences in
641:
547:immediately after the collapse of the
275:
9688:
9581:Coupled Model Intercomparison Project
9406:
9111:
8847:
8407:
8319:
8200:
8152:
8114:
7853:
6839:from the original on 14 November 2022
6124:from the original on 20 December 2023
5645:
4730:from the original on 16 February 2020
4004:from the original on 16 February 2020
3153:Journal of Physics: Conference Series
3144:
1771:
1421:, appear to have a 7,000–10,000-year
198:Lockheed P-38 Lightning fighter plane
9603:Representative Concentration Pathway
8554:Tipping points in the climate system
8230:Carbon dioxide in Earth's atmosphere
7854:Naish, Timothy; et al. (2009).
7318:
7256:
6560:from the original on 24 October 2022
6520:from the original on 22 October 2022
6487:from the original on 8 November 2023
6296:Gautier, Agnieszka (29 March 2023).
6157:from the original on 7 December 2023
6059:from the original on 8 November 2020
5762:from the original on 30 October 2017
5734:from the original on 7 December 2023
5699:from the original on 7 December 2023
5666:from the original on 30 October 2017
5468:
5316:"Antarctic cooling, global warming?"
4268:
2041:. Vol. 88. pp. C41B–0474.
1525:levels to have been more important.
1473:of Antarctica toward the end of the
9374:Nationally determined contributions
9084:Individual action on climate change
8299:World energy supply and consumption
6335:Earth and Planetary Science Letters
6030:Earth and Planetary Science Letters
5471:"Antarctic Ice Mass Loss 2002–2023"
5357:from the original on April 11, 2009
5114:npj Climate and Atmospheric Science
4271:"Antarctic Ice Mass Loss 2002–2023"
3298:npj Climate and Atmospheric Science
1868:Dynamics of Ice Sheets and Glaciers
872:and dilutes the formation of salty
41:One of Earth's two ice sheets: The
24:
9513:Fixed anvil temperature hypothesis
8140:
5200:Vizcarra, Natasha (25 June 2018).
4023:Davies, Bethan (21 October 2020).
3937:Davies, Bethan (21 October 2020).
1650: – Planet with an icy surface
1211:, or about 12% of the area of the
1043:have proven that the warming over
52:and is the largest single mass of
25:
10359:
9440:Satellite temperature measurement
9045:forestry for carbon sequestration
8336:History of climate change science
8091:
7257:Kerr, Richard A. (14 July 1978).
6870:from the original on 18 July 2023
6303:National Snow and Ice Data Center
5206:National Snow and Ice Data Center
1835:from the original on 21 June 2020
1561:While there is evidence of large
1517:of some size. The opening of the
1495:Eocene–Oligocene extinction event
1006:Amundsen–Scott South Pole Station
125:In previous geologic time spans (
9666:
9654:
9643:
9642:
9630:
9291:Climate Change Performance Index
8046:
7904:
7847:
7785:
7750:
7699:
7638:
7613:
7594:
7529:
7472:
7412:
7378:
7335:
7312:
7250:
7144:
7087:
6989:
6954:
6310:from the original on 28 May 2023
2526:Vaughan, David G. (2008-08-20).
1545:This section is an excerpt from
1453:This section is an excerpt from
1190:This section is an excerpt from
1098:
964:This section is an excerpt from
937:
773:This section is an excerpt from
730:
647:This section is an excerpt from
208:
9430:Instrumental temperature record
9381:Sustainable Development Goal 13
8000:10.1016/j.gloplacha.2014.01.012
7319:Buis, Alan (27 February 2020).
6143:Robinson, Ben (15 April 2019).
3899:
3892:10.1016/j.quascirev.2023.108287
3824:
3763:
3740:
3703:
3670:
3643:
3433:
3223:
3162:10.1088/1742-6596/2152/1/012057
2975:
2923:
2874:
2825:
2765:
2665:
2595:
2577:
2519:
2468:
2392:
1866:Greve, R.; Blatter, H. (2009).
1811:"About the Greenland Ice Sheet"
1417:, named after their discoverer
1203:(680 mi) at a latitude of
1041:instrumental temperature record
230:The motion of ice in Antarctica
9498:Climate variability and change
8848:
8539:Retreat of glaciers since 1850
5232:Environmental Research Letters
5016:boundary climate transition".
3145:Zhang, Zhe (7 November 2021).
2603:"Marine ice sheet instability"
1825:"Glacier Girl: The Back Story"
1817:
1803:
1720:
1702:
1698:. National Science Foundation.
1497:about 34 million years ago. CO
1477:, thawing near the end of the
1434:both Heinrich and D–O events.
868:from WAIS also contributes to
671:Earth's two current ice sheets
637:Earth's current two ice sheets
13:
1:
10328:Snow or ice weather phenomena
9608:Shared Socioeconomic Pathways
9143:Climate emergency declaration
6983:10.1016/j.chemgeo.2012.05.024
5287:Davidson, Keay (2002-02-04).
3747:Perkins, Sid (17 June 2021).
1799:. Cambridge University Press.
1678:
1167:2,400 km (1,500 mi)
907:, some have instead proposed
785:(WAIS) is the segment of the
87:. Ice sheets are bigger than
9591:IPCC Sixth Assessment Report
8817:Middle East and North Africa
8153:
8040:10.1016/j.palaeo.2013.09.019
7364:10.1016/0033-5894(88)90057-9
7283:10.1126/science.201.4351.144
7002:Global Biogeochemical Cycles
6150:The University of Manchester
5892:Geophysical Research Letters
5840:Geophysical Research Letters
5155:Geophysical Research Letters
4108:Geophysical Research Letters
3712:Geophysical Research Letters
3623:Geophysical Research Letters
2838:Geophysical Research Letters
2179:Geophysical Research Letters
2132:Geophysical Research Letters
1990:Geophysical Research Letters
862:marine ice sheet instability
559:'s three largest glaciers -
486:IPCC Fifth Assessment Report
454:Marine Ice Cliff Instability
431:Marine ice cliff instability
373:marine ice sheet instability
351:Marine ice sheet instability
27:Large mass of glacial tulips
7:
8320:
7980:Global and Planetary Change
7792:DeConto, Robert M. (2003).
1831:. Smithsonian Institution.
1635:
1617:cooler surface temperatures
1587:passive continental margins
1501:levels were then about 760
1175:1,100 km (680 mi)
1033:misinterpreted by the media
452:A related process known as
203:
164:
10:
10364:
10293:
9425:Global surface temperature
9316:Popular culture depictions
9228:Ecosystem-based adaptation
8958:Carbon capture and storage
8880:Carbon offsets and credits
8201:
7562:10.1038/s41467-022-33310-z
7226:10.1038/s41467-024-47141-7
7177:10.1007/s00248-023-02302-x
7063:10.1038/s41598-018-35054-7
6920:10.1038/s41467-019-11394-4
6356:10.1016/j.epsl.2016.06.053
6050:10.1016/j.epsl.2015.05.018
5956:10.1038/s41586-023-06503-9
5804:10.1038/s41467-018-07206-w
5343:Peter Doran (2006-07-27).
5274:10.1007/s00382-023-06825-4
5127:10.1038/s41612-020-00143-w
4443:10.1038/s41558-023-01818-x
4384:10.1038/s41586-023-05762-w
4186:10.3189/172756501781832340
4025:"West Antarctic Ice Sheet"
3939:"West Antarctic Ice Sheet"
3879:Quaternary Science Reviews
3846:10.1038/s41467-021-23070-7
2444:10.1038/s41467-022-35499-5
2360:10.1038/s41467-018-05003-z
2312:10.1016/j.epsl.2014.12.035
1544:
1511:oxygen isotope ratio cycle
1452:
1369:, which has a much larger
1317:particulate organic carbon
1189:
963:
772:
713:between the three regions.
646:
388:self-reinforcing mechanism
145:. In the same period, the
29:
10343:Effects of climate change
10289:
10208:
10170:
10089:
9994:
9946:
9824:
9793:
9735:
9726:
9637:Climate change portal
9624:
9563:
9530:Extreme event attribution
9448:
9417:
9413:
9402:
9346:
9281:
9203:
9153:School Strike for Climate
9125:
9121:
9107:
9076:
9032:Climate-smart agriculture
8993:
8950:
8860:
8856:
8843:
8767:
8630:
8577:
8420:
8416:
8403:
8326:
8315:
8244:
8213:
8209:
8196:
8179:Climate change adaptation
8174:Climate change mitigation
8169:Effects of climate change
8159:
8148:
7937:10.1038/s41586-018-0155-6
6864:climatetippingpoints.info
6445:10.1038/s41586-020-2742-6
6107:10.1038/s41561-019-0340-8
5604:climatetippingpoints.info
4833:10.1038/s41586-020-2727-5
4602:climatetippingpoints.info
4230:10.1038/s41586-018-0179-y
3463:10.1038/s41586-019-0901-4
3318:10.1038/s41612-020-0121-5
3118:climatetippingpoints.info
2832:Mohajerani, Yara (2018).
2698:10.1038/s41586-018-0179-y
2555:10.1007/s10584-008-9448-3
2254:10.3189/S0022143000023327
1876:10.1007/978-3-642-03415-2
1599:Later uplift, during the
1442:Dansgaard–Oeschger events
1431:Dansgaard–Oeschger events
1179:
1171:
1163:
1155:
1116:
1106:
1097:
1086:
1081:
953:
945:
936:
931:
920:interventions in history.
762:
754:
746:
738:
729:
724:
683:Antarctic mountain ranges
308:. Those ice shelves then
9540:Global warming potential
9347:International agreements
8994:Preserving and enhancing
8438:Arctic methane emissions
8360:Years in climate change
8267:Greenhouse gas emissions
8164:Causes of climate change
6699:Summary for Policymakers
5245:10.1088/1748-9326/acd8d4
1829:Air & Space Magazine
1786:Sections 4.5 and 4.6 of
1613:orographic precipitation
1398:, which are patterns in
1371:global warming potential
1345:carbon dioxide emissions
1313:dissolved organic carbon
1233:greenhouse gas emissions
1222:Greenland has had major
994:Transantarctic Mountains
990:West Antarctic Ice Sheet
974:East Antarctic Ice Sheet
966:East Antarctic Ice Sheet
932:East Antarctic ice sheet
925:East Antarctic ice sheet
858:East Antarctic ice sheet
852: in) to the global
799:Transantarctic Mountains
783:West Antarctic Ice Sheet
775:West Antarctic Ice Sheet
725:West Antarctic ice sheet
718:West Antarctic ice sheet
695:West Antarctic ice sheet
691:East Antarctic ice sheet
45:covers about 98% of the
9571:Climate change scenario
9223:Disaster risk reduction
8875:Carbon emission trading
8685:U.S. insurance industry
8665:Civilizational collapse
8512:sea surface temperature
7671:10.1126/science.1203909
7447:10.1073/pnas.1902469117
6799:10.1126/science.abn7950
6752:10.1126/science.ade4248
6666:10.1073/pnas.1904242116
6347:2016E&PSL.451....1Y
6256:10.1073/pnas.2021442118
6042:2015E&PSL.424..295C
5556:10.1126/science.abn7950
5294:San Francisco Chronicle
4549:10.1126/science.abn7950
4505:10.1126/science.ade0664
3792:10.1126/science.abf6271
3600:10.5194/tc-16-1979-2022
3065:10.1126/science.abn7950
2908:10.5194/tc-12-2869-2018
2399:David Docquier (2016).
2303:2015E&PSL.412..112P
2173:Scambos, T. A. (2004).
2094:10.1126/science.1200109
1955:10.1126/science.1087231
1760:IPCC, 2021: Annex VII:
1341:climate change feedback
569:Kangerdlugssuaq Glacier
9564:Research and modelling
9248:Nature-based solutions
9068:Nature-based solutions
9010:Carbon dioxide removal
8927:Fossil fuel divestment
8912:Climate risk insurance
8822:Small island countries
8443:Arctic sea ice decline
8080:10.5194/cp-11-369-2015
6704:11 August 2021 at the
6608:10.1126/sciadv.aav9396
5639:10.1126/sciadv.abf7787
5030:10.1126/science.aab066
4888:10.1126/sciadv.aaw4132
4651:10.1126/sciadv.abf7787
4331:10.1126/sciadv.aap9467
3921:10.1126/sciadv.adf0198
3256:10.1126/sciadv.aao7212
3008:10.1126/sciadv.1701681
2650:10.5194/tc-12-521-2018
1558:
1486:
1391:
1381:In geologic timescales
1320:
874:Antarctic bottom water
540:
449:
407:
359:proposed that because
314:circumpolar deep water
297:
289:
252:(Milankovich cycles).
231:
218:
177:
57:
9525:Earth's energy budget
9408:Background and theory
9296:Climate crisis (term)
8968:Fossil fuel phase-out
8862:Economics and finance
8827:by individual country
8769:By country and region
8744:Security and conflict
8739:Psychological impacts
8428:Abrupt climate change
8351:Charles David Keeling
8184:By country and region
7542:Nature Communications
7485:Nature Communications
7214:Nature Communications
7120:10.1038/ismej.2014.59
6900:Nature Communications
5792:Nature Communications
5438:Journal of Glaciology
5073:10.5194/tc-7-375-2013
4983:10.5194/tc-7-375-2013
4756:Nature Communications
4712:10.5194/tc-7-375-2013
4422:Nature Climate Change
4165:Journal of Glaciology
4159:Rignot, Eric (2001).
4029:AntarcticGlaciers.org
3986:10.5194/tc-7-375-2013
3943:AntarcticGlaciers.org
3834:Nature Communications
2607:AntarcticGlaciers.org
2424:Nature Communications
2340:Nature Communications
2241:Journal of Glaciology
2235:Weertman, J. (1974).
1654:Quaternary glaciation
1556:
1464:
1388:
1329:microbial communities
1308:
1217:scientific literature
1037:climate change denial
876:, which destabilizes
787:continental ice sheet
685:, and sparse coastal
534:
517:seabed gouging by ice
444:
401:
375:(MISI) would occur.
369:Archimedes' principle
295:
283:
229:
216:
172:
40:
10296:Geographical feature
10132:Volcanic crater lake
9354:Glasgow Climate Pact
9015:Carbon sequestration
8590:Mass mortality event
7627:. September 13, 2009
7023:10.1029/2008gb003327
5904:10.1029/2022GL101827
5898:(6): e2022GL101827.
5860:10.1029/2020GL090471
5846:(5): e2020GL090471.
5730:. 14 December 2017.
5695:. 14 December 2017.
5469:NASA (7 July 2023).
5176:10.1029/2018GL078133
4927:. pp. 125–140.
4269:NASA (7 July 2023).
4128:10.1029/2022GL099543
3724:10.1029/2019GL084183
3718:(4): e2022GL102400.
3664:10.1029/2019JF005054
3636:10.1029/2022GL102400
3629:(4): e2022GL102400.
3417:10.1029/2019JF005418
3378:10.1029/2021EF002576
3364:(4): e2021EF002576.
2859:10.1029/2018GL078173
2200:10.1029/2004GL020670
2152:10.1029/2006GL028154
2011:10.1029/2002GL016329
1666:Wisconsin glaciation
1581:, during the middle
1407:Laurentide Ice Sheet
1301:Role in carbon cycle
1264: in) to global
1088:Grønlands indlandsis
976:(EAIS) lies between
870:ocean stratification
821:that drain into the
711:glacier mass balance
662:covering 98% of the
394:Vulnerable locations
284:The collapse of the
155:Patagonian Ice Sheet
139:Laurentide Ice Sheet
135:Last Glacial Maximum
9493:Climate sensitivity
9268:The Adaptation Fund
8724:Infectious diseases
8631:Social and economic
8071:2015CliPa..11..369K
8059:Climate of the Past
8032:2013PPP...392..161S
7992:2014GPC...116...91J
7929:2018Natur.558..284S
7882:10.1038/nature07867
7874:2009Natur.458..322N
7825:10.1038/nature01290
7817:2003Natur.421..245D
7771:1996Geo....24..163D
7728:10.1038/nature03135
7720:2005Natur.433...53C
7663:2011Sci...334.1261P
7657:(6060): 1261–1264.
7554:2022NatCo..13.5526B
7505:10.1038/ncomms11509
7497:2016NatCo...711509C
7438:2020PNAS..117.3996T
7356:1988QuRes..29..142H
7344:Quaternary Research
7275:1978Sci...201..144K
7169:2023MicEc..86.3057Z
7112:2014ISMEJ...8.2305D
7055:2018NatSR...816623C
7014:2009GBioC..23.2023T
6975:2012ChGeo.320...80R
6912:2019NatCo..10.3567W
6744:2023Sci...381..330C
6715:26 May 2023 at the
6657:2019PNAS..116.9239M
6600:2019SciA....5.9396A
6437:2020Natur.586...70B
6393:10.1038/nature13456
6385:2014Natur.510..525R
6247:2021PNAS..11821442C
6241:(13): e2021442118.
6199:10.1038/nature13456
6191:2014Natur.510..525R
6099:2019NatGe..12..361K
5948:2023Natur.622..528B
5852:2021GeoRL..4890471N
5758:. 24 October 2023.
5755:Greenland Ice Sheet
5662:. 24 October 2023.
5659:Greenland Ice Sheet
5506:10.1038/nature11621
5498:2012Natur.491..586K
5403:10.1038/nature07669
5395:2009Natur.457..459S
5167:2018GeoRL..45.6124S
5064:2013TCry....7..375F
4974:2013TCry....7..375F
4880:2019SciA....5.4132F
4825:2020Natur.585..538G
4776:10.1038/ncomms10325
4768:2016NatCo...710325H
4703:2013TCry....7..375F
4643:2021SciA....7.7787P
4497:2023Sci...382.1384L
4491:(6677): 1384–1389.
4434:2023NatCC..13.1222N
4376:2023Natur.615..841L
4222:2018Natur.558..219I
4177:2001JGlac..47..213R
4120:2022GeoRL..4999543D
4070:10.1038/nature07669
4062:2009Natur.457..459S
3977:2013TCry....7..375F
3784:2021Sci...372.1342B
3778:(6548): 1342–1344.
3542:10.1038/nature24458
3534:2017Natur.550..506W
3455:2019Natur.566...58E
3370:2022EaFut..1002576S
3310:2020npjCA...3...18H
3248:2018SciA....4.7212D
3201:10.1038/nature17145
3193:2016Natur.531..591D
3000:2017SciA....3E1681G
2951:2018GSLSP.461..175R
2899:2018TCry...12.2869G
2850:2018GeoRL..45.7010M
2795:10.1038/nature10114
2787:2011Natur.474...72Y
2690:2018Natur.558..219I
2672:IMBIE team (2018).
2641:2018TCry...12..521G
2547:2008ClCh...91...65V
2489:1978Natur.271..321M
2436:2022NatCo..13.7840D
2352:2018NatCo...9.2728P
2191:2004GeoRL..3118402S
2144:2007GeoRL..34.2602W
2086:2011Sci...331.1592B
2080:(6024): 1592–1595.
2047:2007AGUFM.C41B0474K
2002:2003GeoRL..30.1361A
1949:(5636): 1087–1089.
1913:2005AREPS..33..247C
1396:Milankovitch cycles
1213:Antarctic ice sheet
1200:Greenland ice sheet
1192:Greenland ice sheet
1136: /
1082:Greenland ice sheet
1075:Greenland ice sheet
1002:South Magnetic Pole
986:Greenland ice sheet
905:Pine Island Glacier
797:on the side of the
699:Antarctic Peninsula
660:continental glacier
656:Antarctic ice sheet
649:Antarctic ice sheet
642:Antarctic ice sheet
557:Greenland ice sheet
513:Pine Island Glacier
325:Antarctic Peninsula
276:Boundary conditions
174:Greenland ice sheet
131:Last Glacial Period
85:Greenland ice sheet
81:Antarctic ice sheet
70:continental glacier
43:Antarctic ice sheet
32:Continental Glacier
9064:(LULUCF and AFOLU)
9036:Forest management
9020:Direct air capture
8985:Sustainable energy
8942:Net zero emissions
8937:Low-carbon economy
8932:Green Climate Fund
8719:Indigenous peoples
8622:Plant biodiversity
8410:Effects and issues
7606:2012-06-16 at the
7396:10.1029/GM112p0035
7043:Scientific Reports
6793:(6611): eabn7950.
5451:10.1017/jog.2021.8
5350:The New York Times
5345:"Cold, Hard Facts"
4543:(6611): eabn7950.
3059:(6611): eabn7950.
1714:2012-06-23 at the
1559:
1487:
1413:. These so-called
1392:
1321:
803:Western Hemisphere
541:
528:to ~11,200 B.P.)
450:
408:
298:
290:
266:supraglacial lakes
232:
219:
178:
176:as seen from space
149:ice sheet covered
120:supraglacial lakes
68:, also known as a
58:
18:Ice-sheet dynamics
10305:
10304:
10216:Artificial island
10122:Submarine volcano
10031:Continental shelf
9998:coastal landforms
9794:Continental plain
9729:List of landforms
9682:
9681:
9620:
9619:
9616:
9615:
9555:Radiative forcing
9398:
9397:
9394:
9393:
9218:Adaptive capacity
9103:
9102:
9099:
9098:
8963:Energy transition
8839:
8838:
8835:
8834:
8559:Tropical cyclones
8485:Urban heat island
8399:
8398:
8311:
8310:
8307:
8306:
8272:Carbon accounting
8226:Greenhouse effect
8192:
8191:
7923:(7709): 284–287.
7868:(7236): 322–328.
7811:(6920): 245–249.
7405:978-0-87590-095-7
7269:(4351): 144–146.
7157:Microbial Ecology
7106:(11): 2305–2316.
6738:(6655): 330–335.
6651:(19): 9239–9244.
6379:(7506): 525–528.
6185:(7506): 525–528.
6087:Nature Geoscience
5942:(7983): 528–536.
5492:(7425): 586–589.
5389:(7228): 459–462.
5161:(12): 6124–6133.
4942:978-0-309-11854-5
4819:(7826): 538–544.
4428:(11): 1222–1228.
4370:(7954): 841–847.
4216:(7709): 219–222.
4210:Nature Geoscience
4056:(7228): 459–462.
3528:(7677): 506–510.
3187:(7596): 591–597.
2844:(14): 7010–7018.
2684:(7709): 219–222.
2483:(5643): 321–325.
1885:978-3-642-03414-5
1579:million years ago
1411:ice rafted debris
1187:
1186:
961:
960:
918:civil engineering
894:Isostatic rebound
801:that lies in the
793:, the portion of
770:
769:
595:Last Interglacial
507:(the location of
497:Last Interglacial
442:
357:Johannes Weertman
323:ice shelf in the
227:
157:covered southern
16:(Redirected from
10355:
10251:Land reclamation
10147:Volcanic plateau
9709:
9702:
9695:
9686:
9685:
9670:
9669:
9658:
9657:
9646:
9645:
9635:
9634:
9633:
9598:Paleoclimatology
9415:
9414:
9404:
9403:
9165:Ecological grief
9148:Climate movement
9123:
9122:
9109:
9108:
9089:Plant-based diet
8980:Renewable energy
8858:
8857:
8845:
8844:
8680:Economic impacts
8612:Invasive species
8468:Coastal flooding
8418:
8417:
8405:
8404:
8341:Svante Arrhenius
8317:
8316:
8287:from agriculture
8277:Carbon footprint
8262:Greenhouse gases
8211:
8210:
8198:
8197:
8150:
8149:
8135:
8128:
8121:
8112:
8111:
8085:
8084:
8082:
8050:
8044:
8043:
8013:
8004:
8003:
7974:
7965:
7964:
7908:
7902:
7901:
7851:
7845:
7844:
7802:
7789:
7783:
7782:
7754:
7748:
7747:
7703:
7697:
7696:
7694:
7693:
7642:
7636:
7635:
7633:
7632:
7617:
7611:
7598:
7592:
7591:
7573:
7533:
7527:
7526:
7516:
7476:
7470:
7469:
7459:
7449:
7432:(8): 3996–4006.
7416:
7410:
7409:
7382:
7376:
7375:
7339:
7333:
7332:
7330:
7328:
7316:
7310:
7309:
7307:
7305:
7254:
7248:
7247:
7237:
7205:
7199:
7198:
7188:
7163:(4): 3057–3067.
7148:
7142:
7141:
7131:
7100:The ISME Journal
7091:
7085:
7084:
7074:
7034:
7028:
7027:
7025:
6993:
6987:
6986:
6963:Chemical Geology
6958:
6952:
6951:
6941:
6931:
6891:
6880:
6879:
6877:
6875:
6855:
6849:
6848:
6846:
6844:
6810:
6778:
6772:
6771:
6726:
6720:
6695:
6689:
6688:
6678:
6668:
6636:
6630:
6629:
6619:
6588:Science Advances
6579:
6570:
6569:
6567:
6565:
6559:
6548:
6538:Fox-Kemper, B.;
6535:
6529:
6528:
6526:
6525:
6503:
6497:
6496:
6494:
6492:
6471:
6465:
6464:
6419:
6413:
6412:
6367:
6361:
6360:
6358:
6326:
6320:
6319:
6317:
6315:
6293:
6287:
6286:
6276:
6258:
6225:
6219:
6218:
6173:
6167:
6166:
6164:
6162:
6140:
6134:
6133:
6131:
6129:
6123:
6084:
6075:
6069:
6068:
6066:
6064:
6058:
6027:
6018:
6009:
6008:
6005:10013/epic.38391
5987:
5978:
5977:
5967:
5927:
5916:
5915:
5886:
5880:
5879:
5835:
5826:
5825:
5815:
5783:
5772:
5771:
5769:
5767:
5750:
5744:
5743:
5741:
5739:
5720:
5709:
5708:
5706:
5704:
5685:
5676:
5675:
5673:
5671:
5654:
5643:
5642:
5627:Science Advances
5621:
5615:
5614:
5612:
5610:
5595:
5586:
5585:
5567:
5535:
5526:
5525:
5481:
5475:
5474:
5466:
5460:
5459:
5453:
5444:(263): 533–559.
5429:
5423:
5422:
5372:
5366:
5365:
5363:
5362:
5340:
5334:
5333:
5327:
5326:
5311:
5305:
5304:
5302:
5301:
5284:
5278:
5277:
5262:Climate Dynamics
5256:
5250:
5249:
5247:
5223:
5217:
5216:
5214:
5212:
5197:
5191:
5190:
5188:
5178:
5146:
5140:
5139:
5129:
5105:
5096:
5095:
5085:
5075:
5043:
5034:
5033:
5012:
5006:
5005:
4995:
4985:
4953:
4947:
4946:
4916:
4910:
4909:
4899:
4868:Science Advances
4859:
4853:
4852:
4804:
4798:
4797:
4787:
4746:
4740:
4739:
4737:
4735:
4729:
4714:
4688:
4679:
4673:
4672:
4662:
4631:Science Advances
4622:
4613:
4612:
4610:
4608:
4593:
4587:
4586:
4560:
4531:
4525:
4524:
4479:
4473:
4472:
4462:
4456:
4455:
4445:
4413:
4404:
4403:
4359:
4353:
4352:
4342:
4319:Science Advances
4310:
4304:
4303:
4297:
4287:Fox-Kemper, B.;
4284:
4275:
4274:
4266:
4260:
4259:
4241:
4205:
4199:
4198:
4188:
4171:(157): 213–222.
4156:
4150:
4149:
4139:
4105:
4096:
4090:
4089:
4039:
4033:
4032:
4020:
4014:
4013:
4011:
4009:
4003:
3988:
3962:
3953:
3947:
3946:
3934:
3925:
3924:
3909:Science Advances
3903:
3897:
3896:
3894:
3869:
3860:
3859:
3857:
3828:
3822:
3821:
3803:
3767:
3761:
3760:
3758:
3756:
3744:
3738:
3737:
3735:
3707:
3701:
3700:
3698:
3696:10.1130/G45880.1
3674:
3668:
3667:
3658:(7): 1899–1918.
3647:
3641:
3640:
3638:
3614:
3605:
3604:
3602:
3593:(5): 1979–1996.
3578:
3569:
3568:
3566:
3560:. Archived from
3519:
3510:
3501:
3500:
3474:
3437:
3431:
3430:
3428:
3411:(7): 1899–1918.
3399:
3382:
3381:
3355:
3346:
3340:
3339:
3329:
3292:
3286:
3285:
3275:
3236:Science Advances
3227:
3221:
3220:
3176:
3167:
3166:
3164:
3142:
3129:
3128:
3126:
3124:
3109:
3103:
3102:
3076:
3044:
3038:
3037:
3027:
2994:(11): e1701681.
2988:Science Advances
2979:
2973:
2972:
2962:
2936:
2927:
2921:
2920:
2910:
2893:(9): 2869–2882.
2878:
2872:
2871:
2861:
2829:
2823:
2822:
2769:
2763:
2762:
2756:
2746:Fox-Kemper, B.;
2743:
2734:
2733:
2669:
2663:
2662:
2652:
2620:
2611:
2610:
2599:
2593:
2592:
2581:
2575:
2574:
2532:
2523:
2517:
2516:
2497:10.1038/271321a0
2472:
2466:
2465:
2455:
2415:
2409:
2408:
2396:
2390:
2389:
2379:
2328:
2317:
2316:
2314:
2282:
2267:
2266:
2256:
2232:
2223:
2222:
2212:
2202:
2170:
2164:
2163:
2129:
2120:
2114:
2113:
2068:
2062:
2061:
2059:
2058:
2049:. Archived from
2030:
2024:
2023:
2013:
1981:
1975:
1974:
1934:
1925:
1924:
1896:
1890:
1889:
1863:
1854:
1851:
1845:
1844:
1842:
1840:
1821:
1815:
1814:
1807:
1801:
1800:
1794:
1784:
1769:
1758:
1743:
1742:
1740:
1739:
1730:. Archived from
1724:
1718:
1706:
1700:
1699:
1692:
1419:Hartmut Heinrich
1331:, high rates of
1295:
1294:
1290:
1287:
1278:
1277:
1273:
1263:
1262:
1258:
1255:
1240:ice cliffs calve
1151:
1150:
1148:
1147:
1146:
1141:
1137:
1134:
1133:
1132:
1129:
1102:
1079:
1078:
1056:
1022:greenhouse gases
941:
929:
928:
901:Thwaites Glacier
851:
850:
846:
841:
840:
836:
734:
722:
721:
624:
623:
619:
616:
610:
609:
605:
602:
584:
583:
579:
576:
483:
482:
478:
475:
469:
468:
464:
461:
443:
337:Hektoria Glacier
228:
141:covered much of
21:
10363:
10362:
10358:
10357:
10356:
10354:
10353:
10352:
10308:
10307:
10306:
10301:
10298:
10285:
10221:Artificial reef
10204:
10166:
10142:Volcanic island
10127:Volcanic crater
10085:
10081:Volcanic island
10061:Mid-ocean ridge
9997:
9990:
9942:
9820:
9789:
9731:
9722:
9713:
9683:
9678:
9631:
9629:
9612:
9559:
9550:Orbital forcing
9444:
9409:
9390:
9364:Paris Agreement
9342:
9338:Warming stripes
9277:
9243:Managed retreat
9238:Loss and damage
9199:
9133:Business action
9117:
9095:
9072:
8995:
8989:
8946:
8907:Climate finance
8852:
8831:
8763:
8626:
8602:Extinction risk
8578:Flora and fauna
8573:
8534:Permafrost thaw
8529:Ozone depletion
8458:Extreme weather
8412:
8395:
8322:
8303:
8240:
8205:
8188:
8155:
8144:
8139:
8108:
8094:
8089:
8088:
8051:
8047:
8014:
8007:
7975:
7968:
7909:
7905:
7852:
7848:
7800:
7797:
7790:
7786:
7755:
7751:
7714:(7021): 53–57.
7704:
7700:
7691:
7689:
7643:
7639:
7630:
7628:
7619:
7618:
7614:
7608:Wayback Machine
7599:
7595:
7534:
7530:
7477:
7473:
7417:
7413:
7406:
7383:
7379:
7340:
7336:
7326:
7324:
7317:
7313:
7303:
7301:
7255:
7251:
7206:
7202:
7149:
7145:
7092:
7088:
7035:
7031:
6994:
6990:
6959:
6955:
6892:
6883:
6873:
6871:
6856:
6852:
6842:
6840:
6779:
6775:
6727:
6723:
6717:Wayback Machine
6706:Wayback Machine
6696:
6692:
6637:
6633:
6580:
6573:
6563:
6561:
6557:
6546:
6536:
6532:
6523:
6521:
6504:
6500:
6490:
6488:
6473:
6472:
6468:
6431:(7827): 70–74.
6420:
6416:
6368:
6364:
6327:
6323:
6313:
6311:
6294:
6290:
6226:
6222:
6174:
6170:
6160:
6158:
6141:
6137:
6127:
6125:
6121:
6082:
6076:
6072:
6062:
6060:
6056:
6025:
6019:
6012:
5988:
5981:
5928:
5919:
5887:
5883:
5836:
5829:
5784:
5775:
5765:
5763:
5752:
5751:
5747:
5737:
5735:
5722:
5721:
5712:
5702:
5700:
5687:
5686:
5679:
5669:
5667:
5656:
5655:
5646:
5622:
5618:
5608:
5606:
5596:
5589:
5536:
5529:
5482:
5478:
5467:
5463:
5430:
5426:
5373:
5369:
5360:
5358:
5341:
5337:
5324:
5322:
5312:
5308:
5299:
5297:
5285:
5281:
5257:
5253:
5224:
5220:
5210:
5208:
5198:
5194:
5147:
5143:
5106:
5099:
5044:
5037:
5024:(6281): 76–80.
5013:
5009:
4954:
4950:
4943:
4917:
4913:
4874:(7): eaaw4132.
4860:
4856:
4805:
4801:
4747:
4743:
4733:
4731:
4727:
4686:
4680:
4676:
4623:
4616:
4606:
4604:
4594:
4590:
4532:
4528:
4480:
4476:
4463:
4459:
4414:
4407:
4360:
4356:
4325:(4): eaap9467.
4311:
4307:
4295:
4285:
4278:
4267:
4263:
4206:
4202:
4157:
4153:
4103:
4097:
4093:
4040:
4036:
4021:
4017:
4007:
4005:
4001:
3960:
3954:
3950:
3935:
3928:
3904:
3900:
3870:
3863:
3829:
3825:
3768:
3764:
3754:
3752:
3745:
3741:
3708:
3704:
3675:
3671:
3648:
3644:
3615:
3608:
3579:
3572:
3567:on May 6, 2020.
3564:
3517:
3511:
3504:
3449:(7742): 58–64.
3438:
3434:
3400:
3385:
3353:
3347:
3343:
3293:
3289:
3242:(6): eaao7212.
3228:
3224:
3177:
3170:
3143:
3132:
3122:
3120:
3110:
3106:
3045:
3041:
2980:
2976:
2960:10.1144/sp461.6
2934:
2928:
2924:
2879:
2875:
2830:
2826:
2781:(7349): 72–75.
2770:
2766:
2754:
2744:
2737:
2670:
2666:
2621:
2614:
2601:
2600:
2596:
2583:
2582:
2578:
2535:Climatic Change
2530:
2524:
2520:
2473:
2469:
2416:
2412:
2397:
2393:
2329:
2320:
2283:
2270:
2233:
2226:
2171:
2167:
2127:
2121:
2117:
2069:
2065:
2056:
2054:
2031:
2027:
1982:
1978:
1935:
1928:
1897:
1893:
1886:
1864:
1857:
1852:
1848:
1838:
1836:
1823:
1822:
1818:
1809:
1808:
1804:
1792:
1785:
1772:
1759:
1746:
1737:
1735:
1726:
1725:
1721:
1716:Wayback Machine
1707:
1703:
1694:
1693:
1686:
1681:
1672:Ice-sheet model
1638:
1633:
1632:
1621:atmospheric CO2
1595:above sea level
1585:, when the two
1550:
1542:
1537:
1536:
1524:
1500:
1481:and subsequent
1458:
1450:
1415:Heinrich events
1383:
1363:Russell Glacier
1357:
1310:
1303:
1298:
1297:
1292:
1288:
1285:
1283:
1275:
1271:
1270:
1260:
1256:
1253:
1251:
1248:Paris Agreement
1195:
1144:
1142:
1138:
1135:
1130:
1127:
1125:
1123:
1122:
1090:
1077:
1072:
1071:
1067:ice sheet model
1054:
1051:GRACE satellite
1045:West Antarctica
969:
927:
922:
921:
848:
844:
843:
838:
834:
833:
815:Ronne Ice Shelf
791:West Antarctica
778:
720:
715:
714:
652:
644:
639:
621:
617:
614:
612:
607:
603:
600:
598:
581:
577:
574:
572:
505:West Antarctica
501:Pine Island Bay
480:
476:
473:
471:
466:
462:
459:
457:
435:
433:
404:Pine Island Bay
396:
353:
302:outlet glaciers
278:
221:
211:
206:
167:
151:Northern Europe
127:glacial periods
72:, is a mass of
35:
28:
23:
22:
15:
12:
11:
5:
10361:
10351:
10350:
10345:
10340:
10335:
10330:
10325:
10320:
10303:
10302:
10300:
10299:
10290:
10287:
10286:
10284:
10283:
10278:
10273:
10268:
10263:
10258:
10253:
10248:
10243:
10238:
10233:
10228:
10223:
10218:
10212:
10210:
10206:
10205:
10203:
10202:
10197:
10192:
10187:
10182:
10176:
10174:
10168:
10167:
10165:
10164:
10159:
10154:
10149:
10144:
10139:
10134:
10129:
10124:
10119:
10114:
10109:
10104:
10099:
10093:
10091:
10087:
10086:
10084:
10083:
10078:
10073:
10068:
10066:Oceanic trench
10063:
10058:
10053:
10048:
10043:
10038:
10033:
10028:
10023:
10018:
10013:
10008:
10002:
10000:
9992:
9991:
9989:
9988:
9983:
9978:
9973:
9968:
9963:
9958:
9952:
9950:
9944:
9943:
9941:
9940:
9935:
9930:
9925:
9920:
9919:
9918:
9913:
9903:
9898:
9893:
9888:
9883:
9878:
9877:
9876:
9866:
9861:
9856:
9851:
9846:
9841:
9836:
9830:
9828:
9822:
9821:
9819:
9818:
9813:
9808:
9803:
9797:
9795:
9791:
9790:
9788:
9787:
9782:
9777:
9772:
9767:
9766:
9765:
9755:
9750:
9745:
9739:
9737:
9733:
9732:
9727:
9724:
9723:
9712:
9711:
9704:
9697:
9689:
9680:
9679:
9677:
9676:
9664:
9652:
9640:
9625:
9622:
9621:
9618:
9617:
9614:
9613:
9611:
9610:
9605:
9600:
9595:
9594:
9593:
9583:
9578:
9573:
9567:
9565:
9561:
9560:
9558:
9557:
9552:
9547:
9542:
9537:
9532:
9527:
9522:
9517:
9516:
9515:
9505:
9503:Cloud feedback
9500:
9495:
9490:
9485:
9484:
9483:
9478:
9473:
9468:
9458:
9452:
9450:
9446:
9445:
9443:
9442:
9437:
9432:
9427:
9421:
9419:
9411:
9410:
9400:
9399:
9396:
9395:
9392:
9391:
9389:
9388:
9383:
9378:
9377:
9376:
9371:
9361:
9359:Kyoto Protocol
9356:
9350:
9348:
9344:
9343:
9341:
9340:
9335:
9334:
9333:
9328:
9323:
9313:
9311:Media coverage
9308:
9303:
9301:Climate spiral
9298:
9293:
9287:
9285:
9279:
9278:
9276:
9275:
9270:
9265:
9260:
9255:
9250:
9245:
9240:
9235:
9230:
9225:
9220:
9215:
9209:
9207:
9201:
9200:
9198:
9197:
9192:
9190:Public opinion
9187:
9182:
9177:
9172:
9167:
9162:
9157:
9156:
9155:
9145:
9140:
9138:Climate action
9135:
9129:
9127:
9119:
9118:
9105:
9104:
9101:
9100:
9097:
9096:
9094:
9093:
9092:
9091:
9080:
9078:
9074:
9073:
9071:
9070:
9065:
9059:
9058:
9057:
9052:
9050:REDD and REDD+
9047:
9042:
9034:
9029:
9027:Carbon farming
9024:
9023:
9022:
9017:
9007:
9001:
8999:
8991:
8990:
8988:
8987:
8982:
8977:
8972:
8971:
8970:
8960:
8954:
8952:
8948:
8947:
8945:
8944:
8939:
8934:
8929:
8924:
8919:
8914:
8909:
8904:
8899:
8894:
8889:
8888:
8887:
8877:
8872:
8866:
8864:
8854:
8853:
8841:
8840:
8837:
8836:
8833:
8832:
8830:
8829:
8824:
8819:
8814:
8809:
8804:
8799:
8794:
8789:
8784:
8779:
8773:
8771:
8765:
8764:
8762:
8761:
8759:Water security
8756:
8754:Water scarcity
8751:
8749:Urban flooding
8746:
8741:
8736:
8731:
8726:
8721:
8716:
8711:
8710:
8709:
8699:
8694:
8689:
8688:
8687:
8677:
8672:
8667:
8662:
8657:
8652:
8651:
8650:
8645:
8634:
8632:
8628:
8627:
8625:
8624:
8619:
8614:
8609:
8607:Forest dieback
8604:
8599:
8594:
8593:
8592:
8581:
8579:
8575:
8574:
8572:
8571:
8566:
8561:
8556:
8551:
8546:
8544:Sea level rise
8541:
8536:
8531:
8526:
8525:
8524:
8519:
8517:stratification
8514:
8509:
8504:
8499:
8489:
8488:
8487:
8482:
8472:
8471:
8470:
8460:
8455:
8450:
8445:
8440:
8435:
8430:
8424:
8422:
8414:
8413:
8401:
8400:
8397:
8396:
8394:
8393:
8392:
8391:
8386:
8381:
8376:
8371:
8366:
8358:
8353:
8348:
8343:
8338:
8333:
8327:
8324:
8323:
8313:
8312:
8309:
8308:
8305:
8304:
8302:
8301:
8296:
8295:
8294:
8289:
8284:
8282:Carbon leakage
8279:
8274:
8264:
8259:
8254:
8248:
8246:
8242:
8241:
8239:
8238:
8233:
8223:
8221:Climate system
8217:
8215:
8207:
8206:
8194:
8193:
8190:
8189:
8187:
8186:
8181:
8176:
8171:
8166:
8160:
8157:
8156:
8146:
8145:
8142:Climate change
8138:
8137:
8130:
8123:
8115:
8106:
8105:
8100:
8093:
8092:External links
8090:
8087:
8086:
8065:(3): 369–381.
8045:
8005:
7966:
7903:
7846:
7795:
7784:
7749:
7698:
7637:
7612:
7593:
7528:
7471:
7411:
7404:
7377:
7350:(2): 142–152.
7334:
7311:
7249:
7200:
7143:
7086:
7029:
6988:
6953:
6881:
6850:
6773:
6721:
6690:
6631:
6594:(6): 218–222.
6571:
6530:
6498:
6466:
6414:
6362:
6321:
6288:
6220:
6168:
6135:
6093:(5): 361–368.
6070:
6010:
5999:(3): 141–159.
5993:Polarforschung
5979:
5917:
5881:
5827:
5773:
5745:
5710:
5677:
5644:
5616:
5587:
5527:
5476:
5461:
5424:
5367:
5335:
5306:
5279:
5251:
5218:
5192:
5141:
5097:
5058:(1): 375–393.
5052:The Cryosphere
5035:
5007:
4968:(1): 375–393.
4962:The Cryosphere
4948:
4941:
4933:10.17226/12168
4911:
4854:
4799:
4741:
4691:The Cryosphere
4674:
4614:
4588:
4526:
4474:
4457:
4405:
4354:
4305:
4276:
4261:
4200:
4151:
4091:
4034:
4015:
3965:The Cryosphere
3948:
3926:
3898:
3861:
3823:
3762:
3739:
3702:
3689:(5): 449–452.
3669:
3642:
3606:
3587:The Cryosphere
3570:
3502:
3432:
3383:
3358:Earth's Future
3341:
3287:
3222:
3168:
3130:
3104:
3039:
2974:
2945:(1): 175–186.
2922:
2887:The Cryosphere
2873:
2824:
2764:
2735:
2664:
2635:(2): 521–547.
2629:The Cryosphere
2612:
2594:
2576:
2541:(1–2): 65–79.
2518:
2467:
2410:
2391:
2318:
2268:
2224:
2185:(18): L18402.
2165:
2115:
2063:
2039:Eos Trans. AGU
2025:
1976:
1926:
1907:(1): 247–276.
1891:
1884:
1855:
1846:
1816:
1802:
1770:
1744:
1719:
1701:
1683:
1682:
1680:
1677:
1676:
1675:
1669:
1663:
1660:Snowball Earth
1657:
1651:
1645:
1637:
1634:
1551:
1543:
1541:
1538:
1522:
1498:
1485:re-glaciation.
1459:
1451:
1449:
1446:
1382:
1379:
1375:methanotrophic
1355:
1333:biogeochemical
1302:
1299:
1266:sea level rise
1244:global warming
1196:
1188:
1185:
1184:
1181:
1177:
1176:
1173:
1169:
1168:
1165:
1161:
1160:
1157:
1153:
1152:
1120:
1114:
1113:
1108:
1104:
1103:
1095:
1094:
1084:
1083:
1076:
1073:
1059:Totten Glacier
1029:climate change
970:
962:
959:
958:
955:
951:
950:
947:
943:
942:
934:
933:
926:
923:
854:sea level rise
830:climate change
811:Ross Ice Shelf
779:
771:
768:
767:
764:
760:
759:
756:
752:
751:
748:
744:
743:
740:
736:
735:
727:
726:
719:
716:
653:
645:
643:
640:
638:
635:
526:Before Present
432:
429:
424:Totten Glacier
395:
392:
380:grounding line
355:In the 1970s,
352:
349:
277:
274:
210:
207:
205:
202:
166:
163:
26:
9:
6:
4:
3:
2:
10360:
10349:
10346:
10344:
10341:
10339:
10336:
10334:
10331:
10329:
10326:
10324:
10321:
10319:
10318:Bodies of ice
10316:
10315:
10313:
10297:
10292:
10291:
10288:
10282:
10279:
10277:
10274:
10272:
10269:
10267:
10264:
10262:
10259:
10257:
10254:
10252:
10249:
10247:
10244:
10242:
10239:
10237:
10234:
10232:
10229:
10227:
10224:
10222:
10219:
10217:
10214:
10213:
10211:
10207:
10201:
10198:
10196:
10193:
10191:
10188:
10186:
10183:
10181:
10178:
10177:
10175:
10173:
10169:
10163:
10160:
10158:
10155:
10153:
10152:Volcanic plug
10150:
10148:
10145:
10143:
10140:
10138:
10135:
10133:
10130:
10128:
10125:
10123:
10120:
10118:
10115:
10113:
10110:
10108:
10105:
10103:
10100:
10098:
10095:
10094:
10092:
10088:
10082:
10079:
10077:
10074:
10072:
10069:
10067:
10064:
10062:
10059:
10057:
10054:
10052:
10049:
10047:
10044:
10042:
10039:
10037:
10034:
10032:
10029:
10027:
10024:
10022:
10019:
10017:
10014:
10012:
10009:
10007:
10004:
10003:
10001:
9999:
9993:
9987:
9986:Tunnel valley
9984:
9982:
9979:
9977:
9974:
9972:
9969:
9967:
9964:
9962:
9959:
9957:
9954:
9953:
9951:
9949:
9945:
9939:
9936:
9934:
9931:
9929:
9926:
9924:
9921:
9917:
9914:
9912:
9909:
9908:
9907:
9904:
9902:
9899:
9897:
9894:
9892:
9889:
9887:
9884:
9882:
9879:
9875:
9872:
9871:
9870:
9867:
9865:
9862:
9860:
9857:
9855:
9852:
9850:
9847:
9845:
9842:
9840:
9837:
9835:
9832:
9831:
9829:
9827:
9823:
9817:
9814:
9812:
9809:
9807:
9804:
9802:
9799:
9798:
9796:
9792:
9786:
9783:
9781:
9778:
9776:
9773:
9771:
9768:
9764:
9761:
9760:
9759:
9756:
9754:
9751:
9749:
9746:
9744:
9741:
9740:
9738:
9734:
9730:
9725:
9721:
9717:
9710:
9705:
9703:
9698:
9696:
9691:
9690:
9687:
9675:
9674:
9665:
9663:
9662:
9653:
9651:
9650:
9641:
9639:
9638:
9627:
9626:
9623:
9609:
9606:
9604:
9601:
9599:
9596:
9592:
9589:
9588:
9587:
9584:
9582:
9579:
9577:
9576:Climate model
9574:
9572:
9569:
9568:
9566:
9562:
9556:
9553:
9551:
9548:
9546:
9543:
9541:
9538:
9536:
9533:
9531:
9528:
9526:
9523:
9521:
9518:
9514:
9511:
9510:
9509:
9508:Cloud forcing
9506:
9504:
9501:
9499:
9496:
9494:
9491:
9489:
9486:
9482:
9479:
9477:
9474:
9472:
9469:
9467:
9464:
9463:
9462:
9459:
9457:
9454:
9453:
9451:
9447:
9441:
9438:
9436:
9433:
9431:
9428:
9426:
9423:
9422:
9420:
9416:
9412:
9405:
9401:
9387:
9384:
9382:
9379:
9375:
9372:
9370:
9367:
9366:
9365:
9362:
9360:
9357:
9355:
9352:
9351:
9349:
9345:
9339:
9336:
9332:
9329:
9327:
9324:
9322:
9319:
9318:
9317:
9314:
9312:
9309:
9307:
9304:
9302:
9299:
9297:
9294:
9292:
9289:
9288:
9286:
9284:
9283:Communication
9280:
9274:
9271:
9269:
9266:
9264:
9263:Vulnerability
9261:
9259:
9256:
9254:
9251:
9249:
9246:
9244:
9241:
9239:
9236:
9234:
9233:Flood control
9231:
9229:
9226:
9224:
9221:
9219:
9216:
9214:
9211:
9210:
9208:
9206:
9202:
9196:
9193:
9191:
9188:
9186:
9183:
9181:
9178:
9176:
9173:
9171:
9168:
9166:
9163:
9161:
9158:
9154:
9151:
9150:
9149:
9146:
9144:
9141:
9139:
9136:
9134:
9131:
9130:
9128:
9124:
9120:
9116:
9110:
9106:
9090:
9087:
9086:
9085:
9082:
9081:
9079:
9075:
9069:
9066:
9063:
9060:
9056:
9055:reforestation
9053:
9051:
9048:
9046:
9043:
9041:
9040:afforestation
9038:
9037:
9035:
9033:
9030:
9028:
9025:
9021:
9018:
9016:
9013:
9012:
9011:
9008:
9006:
9003:
9002:
9000:
8998:
8992:
8986:
8983:
8981:
8978:
8976:
8975:Nuclear power
8973:
8969:
8966:
8965:
8964:
8961:
8959:
8956:
8955:
8953:
8949:
8943:
8940:
8938:
8935:
8933:
8930:
8928:
8925:
8923:
8920:
8918:
8915:
8913:
8910:
8908:
8905:
8903:
8900:
8898:
8895:
8893:
8890:
8886:
8883:
8882:
8881:
8878:
8876:
8873:
8871:
8870:Carbon budget
8868:
8867:
8865:
8863:
8859:
8855:
8851:
8846:
8842:
8828:
8825:
8823:
8820:
8818:
8815:
8813:
8810:
8808:
8805:
8803:
8800:
8798:
8795:
8793:
8790:
8788:
8785:
8783:
8780:
8778:
8775:
8774:
8772:
8770:
8766:
8760:
8757:
8755:
8752:
8750:
8747:
8745:
8742:
8740:
8737:
8735:
8732:
8730:
8727:
8725:
8722:
8720:
8717:
8715:
8712:
8708:
8707:Mental health
8705:
8704:
8703:
8700:
8698:
8695:
8693:
8690:
8686:
8683:
8682:
8681:
8678:
8676:
8673:
8671:
8668:
8666:
8663:
8661:
8658:
8656:
8653:
8649:
8648:United States
8646:
8644:
8641:
8640:
8639:
8636:
8635:
8633:
8629:
8623:
8620:
8618:
8615:
8613:
8610:
8608:
8605:
8603:
8600:
8598:
8595:
8591:
8588:
8587:
8586:
8583:
8582:
8580:
8576:
8570:
8567:
8565:
8562:
8560:
8557:
8555:
8552:
8550:
8547:
8545:
8542:
8540:
8537:
8535:
8532:
8530:
8527:
8523:
8520:
8518:
8515:
8513:
8510:
8508:
8505:
8503:
8502:deoxygenation
8500:
8498:
8497:acidification
8495:
8494:
8493:
8490:
8486:
8483:
8481:
8478:
8477:
8476:
8473:
8469:
8466:
8465:
8464:
8461:
8459:
8456:
8454:
8451:
8449:
8446:
8444:
8441:
8439:
8436:
8434:
8431:
8429:
8426:
8425:
8423:
8419:
8415:
8411:
8406:
8402:
8390:
8387:
8385:
8382:
8380:
8377:
8375:
8372:
8370:
8367:
8365:
8362:
8361:
8359:
8357:
8354:
8352:
8349:
8347:
8344:
8342:
8339:
8337:
8334:
8332:
8329:
8328:
8325:
8318:
8314:
8300:
8297:
8293:
8292:from wetlands
8290:
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8280:
8278:
8275:
8273:
8270:
8269:
8268:
8265:
8263:
8260:
8258:
8255:
8253:
8252:Deforestation
8250:
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8237:
8234:
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7011:
7008:(2): GB2023.
7007:
7003:
6999:
6992:
6984:
6980:
6976:
6972:
6969:(13): 80–95.
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5268:: 4623–4641.
5267:
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5255:
5246:
5241:
5238:(6): 064034.
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4289:Hewitt, H. T.
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2332:Pattyn, Frank
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2149:
2145:
2141:
2138:(2): L02602.
2137:
2133:
2126:
2119:
2111:
2107:
2103:
2099:
2095:
2091:
2087:
2083:
2079:
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2067:
2053:on 2012-12-28
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2029:
2021:
2017:
2012:
2007:
2003:
1999:
1995:
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1952:
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1757:
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1749:
1734:on 2006-08-29
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1575:Flade Isblink
1572:
1568:
1564:
1555:
1548:
1534:
1530:
1526:
1520:
1519:Drake Passage
1516:
1512:
1508:
1507:tipping point
1504:
1496:
1492:
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1472:
1468:
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1193:
1182:
1178:
1174:
1170:
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1162:
1158:
1154:
1149:
1140:76.7°N 41.2°W
1121:
1119:
1115:
1112:
1109:
1105:
1101:
1096:
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1080:
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935:
930:
919:
914:
910:
909:interventions
906:
902:
897:
895:
890:
886:
881:
879:
875:
871:
867:
863:
859:
855:
842: ±
831:
826:
824:
820:
817:, and outlet
816:
812:
808:
804:
800:
796:
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749:
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650:
634:
632:
628:
596:
590:
588:
570:
566:
562:
558:
554:
550:
546:
545:Crane Glacier
538:
533:
529:
527:
522:
521:Younger Dryas
518:
514:
510:
506:
502:
498:
494:
489:
487:
455:
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391:
389:
385:
381:
376:
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370:
366:
362:
358:
348:
344:
342:
341:Jorum Glacier
338:
334:
333:Green Glacier
330:
329:Crane Glacier
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311:
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294:
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273:
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259:
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242:
238:
215:
209:Glacial flows
201:
199:
195:
190:
187:
183:
175:
171:
162:
160:
159:South America
156:
152:
148:
144:
143:North America
140:
136:
132:
128:
123:
121:
115:
111:
109:
105:
100:
98:
94:
90:
86:
82:
78:
75:
71:
67:
63:
55:
51:
48:
44:
39:
33:
19:
10137:Volcanic dam
9834:Alluvial fan
9800:
9671:
9659:
9647:
9628:
9461:Carbon cycle
9418:Measurements
9113:Society and
8997:carbon sinks
8902:Climate debt
8892:Carbon price
8714:Human rights
8549:Season creep
8507:heat content
8433:Anoxic event
8346:James Hansen
8107:
8062:
8058:
8048:
8023:
8017:
7983:
7979:
7920:
7916:
7906:
7865:
7859:
7849:
7808:
7804:
7787:
7762:
7758:
7752:
7711:
7707:
7701:
7690:. Retrieved
7654:
7650:
7640:
7629:. Retrieved
7624:
7615:
7596:
7545:
7541:
7531:
7491:(1): 11509.
7488:
7484:
7474:
7429:
7425:
7414:
7387:
7380:
7347:
7343:
7337:
7325:. Retrieved
7314:
7302:. Retrieved
7266:
7262:
7252:
7217:
7213:
7203:
7160:
7156:
7146:
7103:
7099:
7089:
7049:(1): 16623.
7046:
7042:
7032:
7005:
7001:
6991:
6966:
6962:
6956:
6903:
6899:
6872:. Retrieved
6863:
6853:
6841:. Retrieved
6808:10871/131584
6790:
6786:
6776:
6735:
6731:
6724:
6697:IPCC, 2021:
6693:
6648:
6644:
6634:
6591:
6587:
6562:. Retrieved
6550:
6540:Hewitt, H.T.
6533:
6522:. Retrieved
6513:Carbon Brief
6511:
6501:
6489:. Retrieved
6478:
6469:
6428:
6424:
6417:
6376:
6372:
6365:
6338:
6334:
6324:
6312:. Retrieved
6301:
6291:
6238:
6234:
6223:
6182:
6178:
6171:
6159:. Retrieved
6148:
6138:
6126:. Retrieved
6090:
6086:
6073:
6061:. Retrieved
6033:
6029:
5996:
5992:
5939:
5935:
5895:
5891:
5884:
5843:
5839:
5795:
5791:
5764:. Retrieved
5754:
5748:
5736:. Retrieved
5701:. Retrieved
5668:. Retrieved
5658:
5630:
5626:
5619:
5607:. Retrieved
5603:
5565:10871/131584
5547:
5543:
5489:
5485:
5479:
5464:
5455:
5441:
5437:
5427:
5386:
5380:
5370:
5359:. Retrieved
5348:
5338:
5329:
5323:. Retrieved
5320:Real Climate
5309:
5298:. Retrieved
5292:
5282:
5265:
5261:
5254:
5235:
5231:
5221:
5209:. Retrieved
5195:
5158:
5154:
5144:
5117:
5113:
5055:
5051:
5021:
5017:
5010:
4965:
4961:
4951:
4924:
4914:
4871:
4867:
4857:
4816:
4812:
4802:
4759:
4755:
4744:
4732:. Retrieved
4694:
4690:
4677:
4634:
4630:
4605:. Retrieved
4601:
4591:
4558:10871/131584
4540:
4536:
4529:
4488:
4484:
4477:
4467:
4460:
4425:
4421:
4367:
4363:
4357:
4322:
4318:
4308:
4299:
4264:
4213:
4209:
4203:
4168:
4164:
4154:
4111:
4107:
4094:
4053:
4047:
4037:
4028:
4018:
4006:. Retrieved
3968:
3964:
3951:
3942:
3912:
3908:
3901:
3882:
3878:
3837:
3833:
3826:
3775:
3771:
3765:
3753:. Retrieved
3742:
3715:
3711:
3705:
3686:
3682:
3672:
3655:
3651:
3645:
3626:
3622:
3590:
3586:
3562:the original
3525:
3521:
3446:
3442:
3435:
3408:
3404:
3361:
3357:
3344:
3327:10356/143900
3301:
3297:
3290:
3239:
3235:
3225:
3184:
3180:
3152:
3147:
3121:. Retrieved
3117:
3107:
3074:10871/131584
3056:
3052:
3042:
2991:
2987:
2977:
2942:
2938:
2925:
2890:
2886:
2876:
2841:
2837:
2827:
2778:
2774:
2767:
2758:
2748:Hewitt, H.T.
2681:
2677:
2667:
2632:
2628:
2606:
2597:
2589:The Atlantic
2588:
2579:
2538:
2534:
2521:
2480:
2476:
2470:
2427:
2423:
2413:
2404:
2394:
2343:
2339:
2294:
2290:
2247:(67): 3–11.
2244:
2240:
2182:
2178:
2168:
2135:
2131:
2118:
2077:
2073:
2066:
2055:. Retrieved
2051:the original
2038:
2028:
1993:
1989:
1979:
1946:
1942:
1904:
1900:
1894:
1870:. Springer.
1867:
1849:
1837:. Retrieved
1828:
1819:
1805:
1796:
1736:. Retrieved
1732:the original
1722:
1704:
1696:"Ice Sheets"
1560:
1488:
1437:
1436:
1427:
1404:
1393:
1360:
1349:
1337:
1325:carbon cycle
1322:
1237:
1221:
1197:
1110:
1091:
1087:
1063:Wilkes Basin
1026:
1010:
971:
885:Paleoclimate
882:
827:
823:Amundsen Sea
789:that covers
780:
697:(WAIS), and
627:paleoclimate
591:
542:
515:) had found
490:
453:
451:
421:
409:
379:
377:
372:
354:
345:
318:
299:
262:
258:spring tides
254:
241:shear stress
233:
194:World War II
191:
179:
124:
116:
112:
101:
69:
65:
59:
9996:Oceanic and
9736:Mountainous
9488:Carbon sink
9466:atmospheric
9331:video games
9005:Blue carbon
8638:Agriculture
8617:Marine life
8564:Water cycle
8522:temperature
8257:Fossil fuel
8026:: 161–176.
7548:(1): 5526.
7220:(1): 2961.
6906:(1): 3567.
6036:: 295–305.
5868:2268/301943
5798:(1): 4755.
5186:1874/367883
4239:1874/367877
3855:10023/23200
3801:10023/23422
2706:2268/225208
2430:(1): 7840.
2346:(1): 2728.
2297:: 112–121.
2210:11603/24296
1996:(7): 1361.
1423:periodicity
1145:76.7; -41.2
1143: /
1118:Coordinates
675:fresh water
631:The Bahamas
587:ice mélange
447:Eric Rignot
416:Pine Island
306:ice shelves
147:Weichselian
108:ice streams
89:ice shelves
10348:Cryosphere
10338:Glaciology
10323:Ice sheets
10312:Categories
10294:See also:
10209:Artificial
10117:Lava field
10036:Coral reef
9864:Floodplain
9520:Cryosphere
9481:permafrost
9253:Resilience
9205:Adaptation
9180:Litigation
9170:Governance
9115:adaptation
8897:Carbon tax
8850:Mitigation
8787:Antarctica
8675:Disability
7986:: 91–114.
7765:(2): 163.
7692:2014-01-28
7631:2023-06-06
7571:2164/19437
6843:22 October
6564:22 October
6524:2022-10-22
6491:5 December
6314:5 December
6161:7 December
6128:7 December
6063:7 December
5738:7 December
5703:7 December
5361:2008-08-14
5325:2008-08-14
5300:2013-04-13
5211:10 January
5083:1808/18763
4993:1808/18763
4697:(1): 390.
3971:(1): 390.
3885:: 108287.
3733:1912/25343
2057:2008-03-04
1738:2006-08-22
1679:References
1648:Ice planet
1642:Cryosphere
1471:glaciation
1469:, showing
1400:insolation
1352:permafrost
1092:Sermersuaq
1018:atmosphere
998:South Pole
795:Antarctica
703:topography
629:data from
561:Jakobshavn
250:centennial
186:Antarctica
104:geothermal
91:or alpine
62:glaciology
10333:Water ice
10271:Reservoir
10162:Wall rock
10112:Lava dome
10071:Peninsula
9981:Ice field
9938:Waterfall
9801:Ice sheet
9780:Tableland
9720:landforms
9535:Feedbacks
9306:Education
8807:Caribbean
8802:Australia
8729:Migration
8692:Fisheries
8643:Livestock
8569:Wildfires
8475:Heat wave
7687:206533232
7580:2041-1723
7372:129842509
6874:2 October
6833:252161375
6817:0036-8075
6768:259985096
6461:222147426
6265:0027-8424
6115:146504179
5912:257774870
5876:233632072
5609:2 October
5582:252161375
5574:0036-8075
5136:222179485
5092:1994-0424
5002:1994-0424
4849:221885420
4762:: 10325.
4734:6 January
4607:2 October
4583:252161375
4567:0036-8075
4521:266436146
4452:264476246
4400:257807573
4195:128683798
4146:251854055
4008:6 January
3810:0036-8075
3755:9 January
3550:0028-0836
3481:1476-4687
3336:218541055
3304:(1): 18.
3264:2375-2548
3217:205247890
3123:2 October
3099:252161375
3083:0036-8075
3016:2375-2548
2969:0305-8719
2917:1994-0416
2868:134054176
2803:0028-0836
2714:0028-0836
2659:1994-0424
2571:154732005
2563:0165-0009
2505:0028-0836
2368:2041-1723
2263:0022-1430
1571:Maniitsoq
1567:Greenland
1479:Oligocene
1209:Greenland
1180:Thickness
1111:Ice sheet
982:168° east
954:Thickness
949:Ice sheet
866:meltwater
807:sea level
755:Thickness
742:Ice sheet
667:continent
664:Antarctic
537:embayment
519:from the
384:embayment
365:sea level
182:Greenland
66:ice sheet
50:continent
47:Antarctic
10231:Building
10195:Sandhill
10185:Dry lake
10090:Volcanic
10076:Seamount
9758:Mountain
9661:Glossary
9649:Category
9471:biologic
9185:Politics
9077:Personal
8782:Americas
8655:Children
8421:Physical
8214:Overview
8154:Overview
7961:49185845
7953:29899483
7898:15213187
7890:19295607
7833:12529638
7736:15635407
7679:22144622
7625:phys.org
7604:Archived
7588:36130952
7523:27167635
7466:32047039
7299:17801827
7244:38580634
7235:10997585
7195:37843656
7186:10640400
7138:24739624
7081:30413774
6948:31417076
6868:Archived
6837:Archived
6825:36074831
6760:37471537
6713:Archived
6702:Archived
6685:31010924
6626:31223652
6555:Archived
6518:Archived
6485:Archived
6453:32999481
6401:24965655
6308:Archived
6283:33723012
6207:24965655
6155:Archived
6119:Archived
6054:Archived
5974:37853149
5965:10584691
5822:30420596
5760:Archived
5732:Archived
5728:BBC News
5697:Archived
5693:BBC News
5664:Archived
5550:(6611).
5514:23086145
5411:19158794
5355:Archived
4906:31328165
4841:32968257
4794:26838462
4725:Archived
4721:13129041
4669:33931453
4575:36074831
4513:38127761
4392:36991191
4349:29675467
4256:49188002
4248:29899482
4078:19158794
3999:Archived
3995:13129041
3818:34140387
3558:29072274
3497:59606547
3489:30728522
3282:29928691
3209:27029274
3091:36074831
3034:29109976
2811:21637255
2730:49188002
2722:29899482
2462:36543787
2386:30013142
2334:(2018).
2219:36917564
2160:30646727
2110:45110037
2102:21385719
2020:53347069
1971:37375591
1963:12934005
1833:Archived
1762:Glossary
1712:Archived
1636:See also
1629:ice caps
1601:Pliocene
1563:glaciers
1533:Ross Sea
1529:Pliocene
1467:Cenozoic
1315:, POC =
1228:ice caps
1224:glaciers
1004:and the
978:45° west
819:glaciers
766:Receding
707:ice flow
693:(EAIS),
679:nunataks
549:Larsen B
509:Thwaites
495:and the
493:Pliocene
412:Thwaites
361:seawater
321:Larsen B
286:Larsen B
237:ablation
204:Dynamics
165:Overview
153:and the
93:glaciers
83:and the
10172:Aeolian
10157:Volcano
10097:Caldera
10051:Isthmus
10041:Estuary
10021:Channel
9976:Glacier
9948:Glacial
9886:Meander
9854:Channel
9826:Fluvial
9770:Plateau
9476:oceanic
9326:fiction
9175:Justice
9126:Society
8734:Poverty
8453:Drought
8321:History
8245:Sources
8067:Bibcode
8028:Bibcode
7988:Bibcode
7945:1905199
7925:Bibcode
7870:Bibcode
7841:4326971
7813:Bibcode
7767:Bibcode
7759:Geology
7716:Bibcode
7659:Bibcode
7651:Science
7550:Bibcode
7514:4865861
7493:Bibcode
7457:7049167
7434:Bibcode
7352:Bibcode
7327:29 July
7304:29 July
7291:1746691
7271:Bibcode
7263:Science
7165:Bibcode
7129:4992074
7108:Bibcode
7072:6226494
7051:Bibcode
7010:Bibcode
6971:Bibcode
6939:6695407
6908:Bibcode
6787:Science
6740:Bibcode
6732:Science
6676:6511040
6653:Bibcode
6617:6584365
6596:Bibcode
6433:Bibcode
6409:4468457
6381:Bibcode
6343:Bibcode
6341:: 1–9.
6274:8020747
6243:Bibcode
6215:4468457
6187:Bibcode
6095:Bibcode
6038:Bibcode
5944:Bibcode
5848:Bibcode
5813:6232173
5544:Science
5522:4414976
5494:Bibcode
5419:4410477
5391:Bibcode
5163:Bibcode
5060:Bibcode
5018:Science
4970:Bibcode
4897:6636986
4876:Bibcode
4821:Bibcode
4785:4742792
4764:Bibcode
4699:Bibcode
4660:8087405
4639:Bibcode
4537:Science
4493:Bibcode
4485:Science
4430:Bibcode
4372:Bibcode
4340:5906079
4218:Bibcode
4173:Bibcode
4116:Bibcode
4086:4410477
4058:Bibcode
3973:Bibcode
3780:Bibcode
3772:Science
3683:Geology
3530:Bibcode
3451:Bibcode
3366:Bibcode
3306:Bibcode
3273:6007161
3244:Bibcode
3189:Bibcode
3053:Science
3025:5665591
2996:Bibcode
2947:Bibcode
2895:Bibcode
2846:Bibcode
2819:4425075
2783:Bibcode
2686:Bibcode
2637:Bibcode
2609:. 2014.
2591:. 2018.
2543:Bibcode
2513:4149290
2485:Bibcode
2453:9772408
2432:Bibcode
2377:6048022
2348:Bibcode
2299:Bibcode
2187:Bibcode
2140:Bibcode
2082:Bibcode
2074:Science
2043:Bibcode
1998:Bibcode
1943:Science
1909:Bibcode
1839:21 June
1605:valleys
1583:Miocene
1515:ice age
1483:Miocene
1367:methane
1291:⁄
1274:⁄
1259:⁄
1131:41°12′W
1128:76°42′N
1055:60 ± 13
988:or the
847:⁄
837:⁄
687:bedrock
681:of the
620:⁄
606:⁄
580:⁄
565:Helheim
479:⁄
465:⁄
245:gravity
97:ice cap
74:glacial
10281:Tunnel
10266:Quarry
10261:Polder
10226:Bridge
10200:Tundra
10180:Desert
10102:Geyser
10056:Lagoon
10046:Island
9961:Cirque
9933:Valley
9923:Strait
9901:Rapids
9874:island
9844:Canyon
9816:Tundra
9811:Steppe
9785:Valley
9456:Albedo
9449:Theory
9160:Denial
8951:Energy
8812:Europe
8792:Arctic
8777:Africa
8702:Health
8697:Gender
8660:Cities
8585:Biomes
8492:Oceans
8480:Marine
8203:Causes
7959:
7951:
7943:
7917:Nature
7896:
7888:
7861:Nature
7839:
7831:
7805:Nature
7744:830008
7742:
7734:
7708:Nature
7685:
7677:
7586:
7578:
7521:
7511:
7464:
7454:
7402:
7370:
7323:. NASA
7297:
7289:
7242:
7232:
7193:
7183:
7136:
7126:
7079:
7069:
6946:
6936:
6831:
6823:
6815:
6766:
6758:
6708:. In:
6683:
6673:
6624:
6614:
6459:
6451:
6425:Nature
6407:
6399:
6373:Nature
6281:
6271:
6263:
6213:
6205:
6179:Nature
6113:
5972:
5962:
5936:Nature
5910:
5874:
5820:
5810:
5766:26 May
5670:26 May
5633:(18).
5580:
5572:
5520:
5512:
5486:Nature
5417:
5409:
5382:Nature
5134:
5090:
5000:
4939:
4904:
4894:
4847:
4839:
4813:Nature
4792:
4782:
4719:
4667:
4657:
4637:(18).
4581:
4573:
4565:
4519:
4511:
4450:
4398:
4390:
4364:Nature
4347:
4337:
4254:
4246:
4193:
4144:
4114:(16).
4084:
4076:
4049:Nature
3993:
3915:(27).
3816:
3808:
3556:
3548:
3522:Nature
3495:
3487:
3479:
3443:Nature
3334:
3280:
3270:
3262:
3215:
3207:
3181:Nature
3097:
3089:
3081:
3032:
3022:
3014:
2967:
2915:
2866:
2817:
2809:
2801:
2775:Nature
2728:
2720:
2712:
2678:Nature
2657:
2569:
2561:
2511:
2503:
2477:Nature
2460:
2450:
2384:
2374:
2366:
2291:Nature
2261:
2217:
2158:
2108:
2100:
2018:
1969:
1961:
1882:
1609:fjords
1591:uplift
1491:Eocene
1475:Eocene
1164:Length
1013:albedo
889:Eemian
813:, the
763:Status
709:, and
567:, and
137:, the
10256:Levee
10246:Ditch
10236:Canal
10107:Guyot
10026:Coast
10006:Atoll
9971:Fjord
9966:Esker
9956:Arête
9928:Swamp
9916:mouth
9911:delta
9906:River
9891:Oasis
9881:Levee
9859:Cliff
9839:Beach
9806:Plain
9775:Ridge
9763:range
9743:Butte
9716:Earth
9673:Index
9435:Proxy
9195:Women
8670:Crime
8597:Birds
8463:Flood
7957:S2CID
7894:S2CID
7837:S2CID
7801:(PDF)
7740:S2CID
7683:S2CID
7368:S2CID
7287:JSTOR
6829:S2CID
6764:S2CID
6558:(PDF)
6547:(PDF)
6457:S2CID
6405:S2CID
6211:S2CID
6122:(PDF)
6111:S2CID
6083:(PDF)
6057:(PDF)
6026:(PDF)
5908:S2CID
5872:S2CID
5578:S2CID
5518:S2CID
5415:S2CID
5132:S2CID
4845:S2CID
4728:(PDF)
4717:S2CID
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