Knowledge (XXG)

Siberian High

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In spite of its immense influence on the weather experienced by a large proportion of the world's population, scientific studies of the Siberian High have been late in coming, though variability of its behavior was observed as early as the 1960s. However, recent studies of observed
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In general, the Siberian High-pressure system begins to build up at the end of August, reaches its peak in the winter, and remains strong until the end of April. Its genesis at the end of the Arctic summer is caused by the convergence of summer air flows being cooled over interior
330:. Other studies have suggested that the strength of the Siberian High shows an inverse correlation with the high-pressure systems over North Africa. Another correlation has been noted, a connection of a weaker Siberian High and 134:). The Siberian High is the strongest semi-permanent high in the northern hemisphere and is responsible for both the lowest temperature in the Northern Hemisphere outside 712: 1094: 1878: 270:
as days shorten. In the process of the Siberian High's formation, the upper-level jet is transferred across northern Eurasia by adiabatic cooling and descending
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have shown that weakening of the Siberian High is a prime driver of warmer winters in almost all of inland extra-tropical Asia and even over most parts of
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Because increased snow and ice cover enhances the Siberian High, the Siberian High was both more intense and located further west during the early
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across Central Asia. The decrease in magnitude of the Siberian High during the Holocene enabled eastward encroachment of westerlies enriched with
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The plot of mean sea level pressure over the winter months shows a large area of high atmospheric pressure in the South of Siberia.
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has also been found to be similarly inversely related to the mean central pressure of the Siberian High over almost all of
257:, Siberian air forms over the cold tundra of Siberia, which does not radiate heat the same way the ice of the Arctic does. 242:
rainfall from the winds it generates. As a result of the Siberian High, coastal winters in the main city of Pacific Russia
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winter, and similar relationships are found in southern China, whilst the opposite correlation exists over the
807: 759:"Holocene vegetation dynamics and associated climate changes in the Altai Mountains of the Arid Central Asia" 2351: 2056: 1506: 1471: 1464: 1377: 706:
Bradák, B.; Újvári, G.; Stevens, T.; Bógalo, M. F.; González, M. I.; Hyodo, M.; Gomez, C. (1 January 2022).
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and generate dry weather across much of the Asian landscape with the exception of regions such as
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Siberian air is generally colder than Arctic air, because unlike Arctic air which forms over the
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Severe winter cold and attendant dry conditions with little snow and few or no glaciers
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and attendant dry conditions with little snow and few or no glaciers across
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Zhang, Dongliang; Chen, Xi; Li, Yaoming; Zhang, Shengrui (15 July 2020).
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are very cold in relation to its latitude and proximity to the ocean.
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The Siberian High affects the weather patterns in most parts of the
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Cohen, Judah; Saito, Kazuyuki; Entekhabi, Dara (January 2001).
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High pressure mass of cold dry air over northeastern Eurasia
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from September until April. It is usually centered on
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It reaches its greatest size and strength in the 53: 45: 37: 32: 763:Palaeogeography, Palaeoclimatology, Palaeoecology 713:Palaeogeography, Palaeoclimatology, Palaeoecology 551:""Record Chill Spreads Deep into Southeast Asia"" 110:when the air temperature near the center of the 182:, the Siberian High is largely replaced by the 1879:List of atmospheric pressure records in Europe 1324: 1088: 823: 423: 421: 419: 302:and significant relationships as far west as 8: 345:as a result of the extensive glaciation of 298:, with the strongest relationship over the 2309: 2242: 2087: 1984: 1331: 1317: 1309: 1305: 1190: 1183: 1174: 1095: 1081: 1073: 1046: 1037: 1026: 926: 830: 816: 808: 733: 675: 618: 577:"Siberian anticyclone | meteorology" 496: 2163:South-West Indian Ocean tropical cyclone 415: 206:: its influence extends as far west as 29: 278:" that outbreak over warmer parts of 222:. It may block or reduce the size of 7: 912:Tropical cyclones and climate change 2136:Mediterranean tropical-like cyclone 2129:North Indian Ocean tropical cyclone 2062:Mediterranean tropical-like cyclone 1945:East Asian-northwest Pacific storms 142:, and the highest pressure, 1083.8 2224:Upper tropospheric cyclonic vortex 2170:Australian region tropical cyclone 274:, which in extreme cases creates " 25: 446:Encyclopedia of world climatology 2445: 2431: 1387: 363: 2184:South Atlantic tropical cyclone 2143:Black Sea tropical-like cyclone 2177:South Pacific tropical cyclone 1940:Continental North Asian storms 1: 114:is often lower than −40  2438:Tropical cyclones portal 1479:Great Sheffield Gale of 1962 1419:Moray Firth fishing disaster 962:Ridiculously Resilient Ridge 783:10.1016/j.palaeo.2020.109744 735:10.1016/j.palaeo.2021.110719 648:Geophysical Research Letters 599:Geophysical Research Letters 477:Geophysical Research Letters 41:Northeastern part of Eurasia 2288:Mesoscale convective vortex 2270:Mesoscale convective system 1872:List of European windstorms 1289:Pacific Northwest windstorm 2552: 2425: 2052:Australian east coast Low 1995:Australian east coast low 1535:1992 New Year's Day Storm 1385: 1308: 1072: 448:by John E. Oliver, 2005, 88: 76: 2526:Climate change in Russia 1563:Boxing Day Storm of 1998 1556:Christmas Eve storm 1997 892:Annular tropical cyclone 306:and as far southeast as 2536:Environment of Mongolia 2352:Multiple-vortex tornado 1791:Friederike (David) 2018 1784:Eleanor (Burglind) 2018 1507:December 1981 windstorm 1465:North Sea flood of 1953 1378:Christmas Flood of 1717 261:Genesis and variability 2293:Line echo wave pattern 2247:Mesoscale ocean eddies 2016:Southern Ocean cyclone 1104:Extratropical cyclones 897:Bar (tropical cyclone) 887:Central dense overcast 531:The East Asian Monsoon 199: 1665:Friedhelm/Bawbag 2011 1528:Burns' Day storm 1990 1412:Night of the Big Wind 1133:Post-tropical cyclone 882:Rapid intensification 433:26 April 2012 at the 384:Arctic dipole anomaly 336:Antarctic oscillation 197: 126:is often above 1,040 2452:Tornadoes portal 2362:Anticyclonic tornado 2330:Low-topped supercell 2108:Cape Verde hurricane 1500:Gale of January 1976 668:10.1029/2000GL011927 620:10.1029/2004GL019465 519:on 21 February 2018. 498:10.1029/2004GL022271 168:Asian part of Russia 124:atmospheric pressure 81:Aziatsky antitsiklon 77:Азиатский антициклон 69:Siberian Anticyclone 18:Siberian anticyclone 2478: /  2154:Southern Hemisphere 2092:Northern Hemisphere 1980:Southern Hemisphere 1935:Western Disturbance 1749:Thomas (Doris) 2017 1521:Great storm of 1987 1486:1968 Scotland storm 1426:Tay Bridge disaster 1405:Great Storm of 1824 1371:Great Storm of 1703 1341:European windstorms 1170:Northern Hemisphere 988:South Atlantic High 976:Southern Hemisphere 952:North American High 930:Northern Hemisphere 775:2020PPP...55009744Z 726:2022PPP...58510719B 660:2001GeoRL..28..299C 611:2004GeoRL..3110201F 489:2005GeoRL..32.5705D 394:North American High 338:(AAO) is stronger. 300:West Siberian Plain 204:Northern Hemisphere 2101:Atlantic hurricane 2057:Lake Huron cyclone 1118:Anticyclonic storm 993:South Pacific High 957:North Pacific High 872:High-pressure area 862:Anticyclonic storm 343:Middle Pleistocene 332:Arctic oscillation 224:low-pressure cells 200: 164:severe winter cold 112:high-pressure area 38:Area of occurrence 2521:Climate of Russia 2516:Climate of Europe 2482:66.883°N 93.467°E 2461: 2460: 2421: 2420: 2417: 2416: 2413: 2412: 2357:Satellite tornado 2232: 2231: 2197: 2196: 2193: 2192: 2117:Pacific hurricane 2033: 2032: 2029: 2028: 1974: 1973: 1918: 1917: 1888: 1887: 1433:Eyemouth disaster 1349:14th-18th century 1297: 1296: 1257: 1256: 1138:Low-pressure area 1016: 1015: 1008:Subtropical ridge 967:Subtropical ridge 877:Low-pressure area 847:Centers of action 539:978-9-812-38769-1 466:D'Arrigo, Rosanne 61: 60: 16:(Redirected from 2543: 2531:Climate of China 2493: 2492: 2490: 2489: 2488: 2483: 2479: 2476: 2475: 2474: 2471: 2450: 2449: 2448: 2436: 2435: 2434: 2310: 2243: 2186: 2179: 2172: 2165: 2155: 2145: 2138: 2131: 2119: 2110: 2103: 2093: 2088: 2000:Black nor'easter 1985: 1981: 1900:Black Sea storms 1881: 1874: 1856: 1849: 1842: 1835: 1828: 1821: 1814: 1807: 1800: 1793: 1786: 1779: 1772: 1765: 1758: 1751: 1744: 1737: 1730: 1723: 1716: 1709: 1702: 1695: 1688: 1681: 1674: 1667: 1660: 1653: 1646: 1639: 1632: 1625: 1618: 1611: 1604: 1586: 1579: 1572: 1565: 1558: 1551: 1544: 1542:Braer Storm 1993 1537: 1530: 1523: 1516: 1509: 1502: 1495: 1488: 1481: 1474: 1467: 1460: 1453: 1435: 1428: 1421: 1414: 1407: 1391: 1380: 1373: 1366: 1359: 1343: 1333: 1326: 1319: 1310: 1306: 1250: 1243: 1225: 1218: 1211: 1204: 1191: 1184: 1180: 1175: 1171: 1097: 1090: 1083: 1074: 1047: 1043: 1038: 1034: 1027: 983:South Polar High 937:North Polar High 927: 832: 825: 818: 809: 802: 801: 799: 797: 754: 748: 747: 737: 703: 697: 696: 694: 692: 679: 639: 633: 632: 622: 596: 590:Fan, Ke (2004). 587: 581: 580: 573: 567: 566: 564: 562: 553:. Archived from 547: 541: 529:Chang Chih-peh, 527: 521: 520: 515:. Archived from 509: 503: 502: 500: 474: 462: 456: 443: 437: 425: 379:Siberian Express 373: 368: 367: 366: 324:Coromandel Coast 160:Krasnoyarsk Krai 90: 78: 30: 21: 2551: 2550: 2546: 2545: 2544: 2542: 2541: 2540: 2511:Climate of Asia 2496: 2495: 2486: 2484: 2480: 2477: 2472: 2469: 2467: 2465: 2464: 2462: 2457: 2446: 2444: 2432: 2430: 2409: 2378: 2299: 2264: 2228: 2189: 2182: 2175: 2168: 2161: 2153: 2148: 2141: 2134: 2127: 2115: 2106: 2099: 2091: 2079: 2071: 2025: 2004: 1979: 1970: 1949: 1914: 1884: 1877: 1870: 1859: 1852: 1845: 1838: 1831: 1824: 1817: 1810: 1803: 1796: 1789: 1782: 1775: 1768: 1761: 1754: 1747: 1740: 1733: 1726: 1719: 1712: 1705: 1698: 1691: 1684: 1677: 1670: 1663: 1656: 1649: 1642: 1635: 1628: 1621: 1614: 1607: 1600: 1589: 1582: 1575: 1568: 1561: 1554: 1547: 1540: 1533: 1526: 1519: 1512: 1505: 1498: 1491: 1484: 1477: 1470: 1463: 1456: 1449: 1438: 1431: 1424: 1417: 1410: 1403: 1392: 1383: 1376: 1369: 1364:Burchardi flood 1362: 1357:Grote Mandrenke 1355: 1344: 1339: 1337: 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1057: 1056: 1054: 1052: 1048: 1045: 1042:Surface-based 1039: 1036: 1033: 1028: 1025: 1023: 1019: 1009: 1006: 1004: 1001: 999: 998:Kalahari High 996: 994: 991: 989: 986: 984: 981: 980: 978: 974: 968: 965: 963: 960: 958: 955: 953: 950: 948: 945: 943: 942:Siberian High 940: 938: 935: 934: 932: 928: 925: 923: 919: 913: 910: 908: 905: 903: 900: 898: 895: 893: 890: 888: 885: 883: 880: 878: 875: 873: 870: 868: 865: 863: 860: 859: 857: 853: 848: 844: 840: 833: 828: 826: 821: 819: 814: 813: 810: 792: 788: 784: 780: 776: 772: 768: 764: 760: 753: 750: 745: 741: 736: 731: 727: 723: 719: 715: 714: 709: 702: 699: 687: 683: 678: 677:1721.1/110326 673: 669: 665: 661: 657: 653: 649: 645: 638: 635: 630: 626: 621: 616: 612: 608: 604: 600: 593: 586: 583: 578: 572: 569: 556: 552: 546: 543: 540: 536: 532: 526: 523: 518: 514: 508: 505: 499: 494: 490: 486: 482: 478: 471: 467: 461: 458: 455: 454:1-402-03264-1 451: 447: 442: 439: 436: 432: 429: 424: 422: 420: 416: 409: 405: 402: 400: 397: 395: 392: 390: 387: 385: 382: 380: 377: 376: 372: 361: 356: 354: 352: 348: 344: 339: 337: 333: 329: 325: 321: 317: 313: 312:Precipitation 309: 305: 301: 297: 293: 289: 283: 281: 277: 273: 269: 260: 258: 256: 252: 247: 245: 241: 238:that receive 237: 233: 229: 225: 221: 217: 213: 209: 205: 196: 189: 187: 185: 181: 178:. During the 177: 173: 169: 165: 161: 157: 153: 149: 145: 141: 137: 133: 129: 125: 121: 117: 113: 109: 105: 101: 97: 94: 86: 82: 74: 70: 66: 65:Siberian High 56: 52: 48: 44: 40: 36: 33:Siberian High 31: 19: 2506:Anticyclones 2463: 2443: 2429: 2342:Funnel cloud 2260:Haida Eddies 2219:Polar vortex 1777:Herwart 2017 1770:Ophelia 2017 1693:St Jude 2013 1672:Joachim 2011 1651:Xynthia 2010 1609:Jeanett 2002 1594:21st century 1514:Charley 1986 1451:Ulysses 1903 1443:20th century 1397:19th century 1274:Hatteras low 1269:Aleutian Low 1209:Colorado low 1143:Weather bomb 941: 843:anticyclones 794:. Retrieved 766: 762: 752: 717: 711: 701: 689:. Retrieved 651: 647: 637: 602: 598: 585: 571: 559:. Retrieved 555:the original 545: 530: 525: 517:the original 507: 480: 476: 460: 445: 441: 404:Aleutian Low 399:Polar vortex 351:water vapour 340: 284: 264: 248: 201: 95: 80: 68: 64: 62: 2485: / 2400:Steam devil 2320:Mesocyclone 2214:Cut-off low 2202:Upper level 2039:Subtropical 2009:Other areas 1954:Other areas 1930:Asiatic Low 1854:Ciarán 2023 1840:Larisa 2023 1833:Eunice 2022 1819:Aurore 2021 1812:Dennis 2020 1798:Adrian 2018 1763:Xavier 2017 1735:Niklas 2015 1686:Andrea 2012 1679:Dagmar 2011 1630:Kyrill 2007 1616:Gudrun 2005 1602:Oratia 2000 1584:Martin 1999 1577:Lothar 1999 1570:Anatol 1999 1472:Debbie 1961 1458:Iberia 1941 1223:Bighorn Low 1194:Lee Cyclone 1187:Continental 947:Azores High 922:Anticyclone 605:(10): n/a. 561:11 December 318:during the 253:around the 244:Vladivostok 232:Caspian Sea 220:Philippines 184:Asiatic low 140:Verkhoyansk 104:Lake Baikal 2500:Categories 2405:Fire whirl 2395:Dust devil 2374:Waterspout 2335:Wall cloud 2047:Kona storm 1966:Kona storm 1847:Babet 2023 1826:Malik 2022 1805:Ciara 2020 1700:Xaver 2013 1658:Berit 2011 1644:Klaus 2009 1279:Nor'easter 902:Superstorm 796:5 November 769:: 109744. 720:: 110719. 691:4 November 629:10289/1741 410:References 276:cold domes 255:North Pole 240:orographic 118:(−40  2369:Landspout 2325:Supercell 2305:Whirlwind 2238:Mesoscale 2021:Sudestada 1988:Australia 1910:Genoa low 1756:Zeus 2017 1742:Egon 2017 1728:Tini 2014 1714:Anne 2014 1707:Dirk 2013 1637:Emma 2008 1549:Lili 1996 1148:Sting jet 907:Hypercane 791:216474621 744:239066555 686:129024923 533:; p. 55. 389:Cold wave 334:when the 328:Sri Lanka 308:Guangdong 280:East Asia 272:advection 234:coast of 136:Greenland 130:(31  128:millibars 2390:Gustnado 2283:Mesohigh 2278:Wake Low 2077:Tropical 1864:See also 1623:Per 2007 1284:Gulf low 1160:Rainband 1111:Concepts 855:Concepts 839:Cyclones 431:Archived 357:See also 230:and the 228:Hokuriku 212:Malaysia 190:Overview 172:Mongolia 150:, 32.01 146:(108.38 2473:93°28′E 2470:66°53′N 2347:Tornado 2123:Typhoon 2082:Outline 2067:Thermal 1262:Oceanic 1128:Cyclone 1022:Cyclone 771:Bibcode 722:Bibcode 656:Bibcode 607:Bibcode 485:Bibcode 304:Hungary 251:sea ice 216:monsoon 122:). The 100:Eurasia 85:Chinese 73:Russian 1961:Arctic 1302:Europe 789:  742:  684:  537:  452:  320:boreal 296:Europe 180:summer 174:, and 108:winter 93:Pinyin 89:西伯利亞高壓 87:: 67:(also 54:Effect 46:Season 2383:Minor 2313:Major 1893:Other 1233:Other 1123:Storm 1051:Polar 867:Storm 787:S2CID 740:S2CID 682:S2CID 595:(PDF) 483:(5). 473:(PDF) 290:over 208:Italy 176:China 156:Agata 154:) at 1923:Asia 1153:List 841:and 798:2022 693:2022 563:2011 535:ISBN 450:ISBN 326:and 292:Asia 236:Iran 152:inHg 144:mbar 132:inHg 63:The 779:doi 767:550 730:doi 718:585 672:hdl 664:doi 625:hdl 615:doi 493:doi 148:kPa 83:); 2502:: 785:. 777:. 765:. 761:. 738:. 728:. 716:. 710:. 680:. 670:. 662:. 652:28 650:. 646:. 623:. 613:. 603:31 601:. 597:. 491:. 481:32 479:. 475:. 418:^ 310:. 282:. 186:. 170:, 158:, 120:°F 116:°C 91:; 75:: 71:; 2084:) 2080:( 1332:e 1325:t 1318:v 1096:e 1089:t 1082:v 849:) 831:e 824:t 817:v 800:. 781:: 773:: 746:. 732:: 724:: 695:. 674:: 666:: 658:: 631:. 627:: 617:: 609:: 579:. 565:. 501:. 495:: 487:: 79:( 20:)

Index

Siberian anticyclone
Russian
Chinese
Pinyin
Eurasia
Lake Baikal
winter
high-pressure area
°C
°F
atmospheric pressure
millibars
inHg
Greenland
Verkhoyansk
mbar
kPa
inHg
Agata
Krasnoyarsk Krai
severe winter cold
Asian part of Russia
Mongolia
China
summer
Asiatic low

Northern Hemisphere
Italy
Malaysia

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