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Cryoconite

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of ice, increasing absorption of heat. Cryoconite is constantly being added to snow and ice formations along with snow. It is buried within the snow or ice, but as the snow or ice melts increasing amounts of dark material is exposed on the surface, accelerating melting.
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when he traveled on Greenland's icecap in 1870. During summer, cryoconite holes frequently contain liquid water and thus provide a niche for cold-adapted microorganisms like bacteria, algae and animals like
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to thrive. Cryoconite typically settles and concentrates at the bottom of these holes creating a noticeable dark mass.
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Fontaneto D; Iakovenko N; De Smet W.H. (2015). "Diversity gradients of rotifer species richness in Antarctica".
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emissions, and soot. It was first described and named by
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made of a combination of small rock particles, soot and
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Woods Hole Image of the Day: Attack of the cryoconites
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Measuring a Cryoconite hole, Longyearbreen glacier (
47:. The darkening, especially from small amounts of 20:A layer of cryoconite on the surface of a glacier. 262: 176: 174: 228: 200: 15: 171: 263: 108:Taking a sample, Longyearbreen glacier 134:from the original on 31 January 2013 75:Soot decreases the reflectivity, or 35:which is deposited and builds up on 13: 250:External links and further reading 128:"The darkening of Arctic glaciers" 14: 287: 197:June 2010, accessed July 8, 2010 182:"Changing Greenland - Melt Zone" 101: 85: 146: 120: 1: 154:"Cryoconite hole information" 7: 10: 292: 130:. Aberystwyth University. 230:10067/1255870151162165141 221:10.1007/s10750-015-2258-5 113: 61:Nils A. E. Nordenskiöld 21: 27:is powdery windblown 19: 194:National Geographic 187:2016-03-03 at the 53:volcanic eruptions 22: 283: 243: 242: 232: 204: 198: 178: 169: 168: 166: 165: 156:. Archived from 150: 144: 143: 141: 139: 124: 105: 89: 291: 290: 286: 285: 284: 282: 281: 280: 261: 260: 252: 247: 246: 205: 201: 189:Wayback Machine 179: 172: 163: 161: 152: 151: 147: 137: 135: 126: 125: 121: 116: 109: 106: 97: 94:Longyear Valley 90: 12: 11: 5: 289: 279: 278: 273: 259: 258: 251: 248: 245: 244: 215:(1): 235–248. 199: 191:page 3, of 4, 170: 145: 118: 117: 115: 112: 111: 110: 107: 100: 98: 91: 84: 9: 6: 4: 3: 2: 288: 277: 274: 272: 269: 268: 266: 257: 254: 253: 240: 236: 231: 226: 222: 218: 214: 210: 209:Hydrobiologia 203: 196: 195: 190: 186: 183: 177: 175: 160:on 2009-11-23 159: 155: 149: 133: 129: 123: 119: 104: 99: 95: 88: 83: 82: 81: 78: 73: 71: 67: 62: 58: 54: 50: 46: 42: 38: 34: 30: 26: 18: 276:Particulates 212: 208: 202: 192: 180:Jenkins, M. 162:. Retrieved 158:the original 148: 136:. Retrieved 122: 74: 24: 23: 70:tardigrades 57:power plant 265:Categories 164:2010-07-08 138:1 February 25:Cryoconite 271:Glaciers 239:17019801 185:Archived 132:Archived 66:rotifers 45:ice caps 41:glaciers 33:microbes 237:  77:albedo 235:S2CID 114:Notes 43:, or 140:2013 68:and 49:soot 37:snow 29:dust 225:hdl 217:doi 213:750 55:or 267:: 233:. 223:. 211:. 173:^ 39:, 241:. 227:: 219:: 167:. 142:. 96:)

Index


dust
microbes
snow
glaciers
ice caps
soot
volcanic eruptions
power plant
Nils A. E. Nordenskiöld
rotifers
tardigrades
albedo
Measuring a Cryoconite hole, Longyearbreen glacier (Longyear Valley)
Longyear Valley
Taking a sample, Longyearbreen glacier
"The darkening of Arctic glaciers"
Archived
"Cryoconite hole information"
the original


"Changing Greenland - Melt Zone"
Archived
Wayback Machine
National Geographic
doi
10.1007/s10750-015-2258-5
hdl
10067/1255870151162165141

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