20:
661:
60:. Extratropical cyclones which form in the sub-polar latitudes in the North Pacific typically slow down and reach maximum intensity in the area of the Aleutian Low. Tropical cyclones that form in the tropical and equatorial regions of the Pacific can veer northward and get caught in the Aleutian Low. This is usually seen in the later summer months. Both the
85:
The low serves as an atmospheric driver for low-pressure systems, post-tropical cyclones and their remnants and can generate strong storms that impact Alaska and Canada. Intensity of the low is strongest in the winter and almost completely dissipates in the summer. The circulation pattern is measured
95:
takes over and breaks apart the
Aleutian Low. This high-pressure circulation pattern strongly influences tropical cyclone paths. The presence of the Eurasian and North American continents prevent a continuous belt of low pressure from developing in the Northern Hemisphere sub-polar latitudes, which
72:
that had dissipated and restrengthened when the systems entered the
Aleutian Low region. The storms are remembered and marked as two of the strongest storms to impact the Bering Sea and Aleutian Islands with pressure dropping below 950 mb in each system. The magnitude of the low pressure creates an
47:
during the
Northern Hemisphere winter. It is a climatic feature centered near the Aleutian Islands measured based on mean sea-level pressure. It is one of the largest atmospheric circulation patterns in the Northern Hemisphere and represents one of the "main centers of action in atmospheric
96:
would mirror the circumpolar belt of low pressure and frequent storms in the
Southern Ocean. However, the presence of the continents disrupts this motion, and the subpolar belt of low pressure is well developed only in the North Pacific (the Aleutian Low) and the North Atlantic (the
100:, which is located between Greenland and Iceland). The strength of the Aleutian Low has been proposed as a driving factor in determining primary production in the water column and, in turn, impacting the catch in the salmon fishery.
90:
help mark the locations of cyclones and their paths over a given time period. However, there is significant variability in these measurements. The circulation pattern shifts during the
Northern Hemisphere summer when the
1216:
1211:
199:"Icelandic Low cyclone activity: Climatological features, linkages with the NAO, and relationships with recent changes in the Northern Hemisphere circulation"
73:
extreme atmospheric disturbance, which can cause other significant shifts in weather. Following the
November 2014 Bering Sea cyclone, a huge cold wave,
1171:
1020:
487:
366:
117:
Rodionov, S.N.; Bond, N.A.; Overland, J.E. (November 2007). "The
Aleutian Low, storm tracks, and winter climate variability in the Bering Sea".
1150:
545:
602:
494:
74:
359:
340:. Topic ed. P.Saundry. Ed.-in-chief C.J.Cleveland. Encyclopedia of Earth. National council for Science and the Environment.
1287:
595:
827:
729:
65:
61:
352:
223:
198:
178:
153:
1327:
243:"The optimal stability 'window': a mechanism underlying decadal fluctuations in North Pacific salmon stocks?"
1232:
806:
690:
588:
242:
1143:
560:
628:
424:
87:
1332:
1317:
1266:
1322:
1041:
834:
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778:
743:
736:
649:
1034:
855:
820:
683:
404:
375:
69:
336:
1055:
771:
750:
254:
210:
165:
126:
8:
1271:
1206:
985:
908:
799:
792:
757:
697:
676:
642:
258:
214:
169:
130:
612:
389:
319:
154:"Objective identification of cyclones and their circulation intensity, and climatology"
92:
992:
764:
704:
409:
311:
270:
266:
36:
936:
301:
262:
218:
173:
134:
40:
290:"Physics to Fish: Interactions Between Physics and Biology on a Variety of Scales"
56:
The
Aleutian Low is characterized by heavily influencing the path and strength of
1048:
943:
922:
880:
635:
473:
1125:
1006:
964:
957:
950:
901:
887:
873:
848:
841:
512:
194:
138:
24:
19:
1311:
1176:
971:
929:
915:
722:
550:
519:
315:
274:
97:
306:
289:
1111:
1104:
1090:
1083:
1069:
1027:
1013:
999:
978:
480:
414:
1201:
1118:
1097:
1076:
1062:
894:
813:
344:
238:
323:
1237:
77:, hit the US bringing record breaking low temperatures to many states.
44:
1292:
1181:
419:
16:
Semi-permanent low-pressure system located near the
Aleutian Islands
660:
555:
431:
399:
57:
394:
224:
10.1175/1520-0442(1997)010<0453:ilcacf>2.0.co;2
179:
10.1175/1520-0434(1997)012<0595:OIOCAT>2.0.CO;2
119:
Deep Sea
Research Part II: Topical Studies in Oceanography
192:
116:
110:
1309:
1151:List of atmospheric pressure records in Europe
596:
360:
603:
589:
374:
367:
353:
305:
222:
177:
151:
18:
610:
287:
237:
1310:
75:November 2014 North American cold wave
584:
348:
1217:East Asian-northwest Pacific storms
13:
14:
1344:
51:
659:
267:10.1046/j.1365-2419.1997.00033.x
66:November 2014 Bering Sea cyclone
62:November 2011 Bering Sea cyclone
1212:Continental North Asian storms
281:
231:
186:
145:
1:
193:Serreze, Mark; Carse, Fiona;
103:
751:Great Sheffield Gale of 1962
691:Moray Firth fishing disaster
197:; Rogers, Jeffery C (1997).
23:A large Aleutian Low in the
7:
1144:List of European windstorms
561:Pacific Northwest windstorm
10:
1349:
139:10.1016/j.dsr2.2007.08.002
80:
1280:
1267:Australian east coast low
1259:
1250:
1225:
1194:
1164:
1135:
865:
807:1992 New Year's Day Storm
714:
668:
657:
620:
580:
573:
533:
504:
465:
458:
449:
440:
382:
835:Boxing Day Storm of 1998
828:Christmas Eve storm 1997
288:Gargett, Ann E. (1997).
1063:Friederike (David) 2018
1056:Eleanor (Burglind) 2018
779:December 1981 windstorm
737:North Sea flood of 1953
650:Christmas Flood of 1717
335:C.Michael Hogan. 2011.
307:10.5670/oceanog.1997.05
158:Weather and Forecasting
152:Sinclair, Mark (1997).
1288:Southern Ocean cyclone
376:Extratropical cyclones
247:Fisheries Oceanography
70:extratropical cyclones
28:
937:Friedhelm/Bawbag 2011
800:Burns' Day storm 1990
684:Night of the Big Wind
405:Post-tropical cyclone
86:based on averages of
22:
1328:Atmospheric dynamics
772:Gale of January 1976
125:(23–26): 2560–2577.
35:is a semi-permanent
1252:Southern Hemisphere
1207:Western Disturbance
1021:Thomas (Doris) 2017
793:Great storm of 1987
758:1968 Scotland storm
698:Tay Bridge disaster
677:Great Storm of 1824
643:Great Storm of 1703
613:European windstorms
442:Northern Hemisphere
259:1997FisOc...6..109G
215:1997JCli...10..453S
170:1997WtFor..12..595S
131:2007DSRII..54.2560R
37:low-pressure system
27:on October 24, 2011
390:Anticyclonic storm
203:Journal of Climate
93:North Pacific High
29:
1305:
1304:
1301:
1300:
1246:
1245:
1190:
1189:
1160:
1159:
705:Eyemouth disaster
621:14th-18th century
569:
568:
529:
528:
410:Low-pressure area
88:synoptic features
39:located near the
1340:
1333:Types of cyclone
1318:Aleutian Islands
1272:Black nor'easter
1257:
1256:
1253:
1172:Black Sea storms
1153:
1146:
1128:
1121:
1114:
1107:
1100:
1093:
1086:
1079:
1072:
1065:
1058:
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1044:
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1016:
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995:
988:
981:
974:
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953:
946:
939:
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918:
911:
904:
897:
890:
883:
876:
858:
851:
844:
837:
830:
823:
816:
814:Braer Storm 1993
809:
802:
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746:
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41:Aleutian Islands
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1323:Weather hazards
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735:
728:
721:
710:
703:
696:
689:
682:
675:
664:
655:
648:
641:
636:Burchardi flood
634:
629:Grote Mandrenke
627:
616:
611:
609:
565:
525:
518:
511:
500:
493:
488:Great basin low
486:
479:
474:Alberta clipper
472:
450:
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436:
378:
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332:
331:
286:
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239:Gargett, Ann E.
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993:Christina 2014
989:
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765:Quimburga 1972
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513:Panhandle hook
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349:
343:
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338:Gulf of Alaska
330:
329:
300:(3): 128–131.
280:
253:(2): 109–117.
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195:Barry, Roger G
185:
164:(3): 595–612.
144:
108:
107:
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82:
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53:
52:Classification
50:
48:circulation."
25:Gulf of Alaska
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1210:
1208:
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1199:
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1183:
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1177:Icelandic Low
1175:
1173:
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1169:
1167:
1163:
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773:
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544:
542:
539:
538:
536:
532:
521:
520:November gale
517:
514:
510:
509:
507:
503:
496:
492:
489:
485:
482:
478:
475:
471:
470:
468:
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461:
457:
454:
451:North America
448:
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159:
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109:
101:
99:
98:Icelandic Low
94:
89:
78:
76:
71:
67:
63:
59:
49:
46:
42:
38:
34:
26:
21:
1049:Herwart 2017
1042:Ophelia 2017
965:St Jude 2013
944:Joachim 2011
923:Xynthia 2010
881:Jeanett 2002
866:21st century
786:Charley 1986
723:Ulysses 1903
715:20th century
669:19th century
546:Hatteras low
541:Aleutian Low
540:
481:Colorado low
415:Weather bomb
337:
297:
294:Oceanography
293:
283:
250:
246:
233:
206:
202:
188:
161:
157:
147:
122:
118:
112:
84:
55:
33:Aleutian Low
32:
30:
1281:Other areas
1226:Other areas
1202:Asiatic Low
1126:Ciarán 2023
1112:Larisa 2023
1105:Eunice 2022
1091:Aurore 2021
1084:Dennis 2020
1070:Adrian 2018
1035:Xavier 2017
1007:Niklas 2015
958:Andrea 2012
951:Dagmar 2011
902:Kyrill 2007
888:Gudrun 2005
874:Oratia 2000
856:Martin 1999
849:Lothar 1999
842:Anatol 1999
744:Debbie 1961
730:Iberia 1941
495:Bighorn Low
466:Lee Cyclone
459:Continental
1312:Categories
1238:Kona storm
1119:Babet 2023
1098:Malik 2022
1077:Ciara 2020
972:Xaver 2013
930:Berit 2011
916:Klaus 2009
551:Nor'easter
209:(3): 455.
104:References
45:Bering Sea
1293:Sudestada
1260:Australia
1182:Genoa low
1028:Zeus 2017
1014:Egon 2017
1000:Tini 2014
986:Anne 2014
979:Dirk 2013
909:Emma 2008
821:Lili 1996
420:Sting jet
316:1042-8275
275:1365-2419
1136:See also
895:Per 2007
556:Gulf low
432:Rainband
383:Concepts
324:43924818
241:(1997).
64:and the
58:cyclones
534:Oceanic
400:Cyclone
255:Bibcode
211:Bibcode
166:Bibcode
127:Bibcode
81:Effects
43:in the
1233:Arctic
574:Europe
322:
314:
273:
1165:Other
505:Other
395:Storm
320:JSTOR
68:were
1195:Asia
425:List
312:ISSN
271:ISSN
31:The
302:doi
263:doi
219:doi
174:doi
135:doi
1314::
318:.
310:.
298:10
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269:.
261:.
249:.
245:.
217:.
207:10
205:.
201:.
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162:12
160:.
156:.
133:.
123:54
121:.
604:e
597:t
590:v
368:e
361:t
354:v
326:.
304::
277:.
265::
257::
251:6
227:.
221::
213::
182:.
176::
168::
141:.
137::
129::
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.