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Cut-off low

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and an ascending motion, especially when they are deepening. A cut-off low can persist from a few days to more than a week. It may be absorbed into the general circulation while another forms in the same place a few days later. The evolution and movement of a cold low, like any
150:. High cold drops, between 1,000 and 10,000 m, are regions of low stability, while low cold drops are regions of relatively stable air. Composed of very cold air of polar origin, it typically has a horizontal extent of 300 to 1000 km and is 5,000 to 10,000 meters above 141:
The diameter of a cut-off low can vary from a few hundred to a thousand kilometers. The air there is homogeneous and without a front line separating it from the surrounding masses, while having a decisive influence on the weather. It then most often leads to an
199:. A cut-off low has a slow movement, typically over a confined region, where it produces heavy rainfall, and can result in severe flooding. For example, a cut-off low was responsible for the 1575: 328:
de la Torre, Laura; Gimeno, Luis; Nieto, Raquel; Ribera, Pedro; Gallego, David; García-Herrera, Ricardo; García, José Agustín; Nuñez, Marcelino; Redaño, Angel; Lorente, Jerónimo (2005).
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that originate from the east. In eastern Australia, a cut-off low can bring accumulating and widespread snowfall at low-level areas and as well as elevated regions in the
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Whilst cut-off lows can form at any time of the year, they are more common in autumn, winter and spring in much of the areas affected, particularly in Australia and the
274: 429: 369:"From the concept of "Kaltlufttropfen" (cold air pool) to the cut-off low. The case of September 1971 in Spain as an example of their role in heavy rainfalls" 1530: 1379: 846: 725: 1509: 904: 961: 853: 106:. Because they are separated from the main westerly flow, cut-off lows can move slowly and erratically. In certain arrangements, known as a 1793: 121:
is brought towards more southern regions (or northern, in the southern hemisphere) by the jet stream moving between 5 and 9 km
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A cut-off low has a slow movement, typically over a confined region, where it produces heavy rainfall. They are volatile,
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in the upper-air flow pinches off and separates into a closed circulation. It is defined by concentric
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Cut off lows typically create unsettled weather and, in the warm season, they may produce a lot of
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By Sarah McPhee and Daniella White from The Daily Telegraph. June 10, 2021
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or a blocking pattern, they can remain in place for long periods of time.
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Sydney shivers through coldest day since 1984 as snow blankets NSW
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Cut-Off Low pressure systems - Meteorological Physical Background
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Cut-Off Low pressure systems - Meteorological Physical Background
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A cut-off low situated over Italy and the tip of northern Libya.
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In southeastern Australia, cut-off lows can be associated with
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Buzz word: 'Cut-off low' to bring rain to DMV most of the week
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which has become completely displaced (cut off) from basic
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In Spain, cut-off lows are often referred to by the name "
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is "cut off"" from the primary westerly winds of the
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(2007). 1510:List of atmospheric pressure records in Europe 187:Effects of a cut-off low of September 1997 in 66:or between 20° and 45°) and can remain nearly 955: 719: 454: 166:systems that meander to the west with strong 962: 948: 733: 726: 712: 461: 447: 1794:South-West Indian Ocean tropical cyclone 182: 132: 18: 969: 2097: 82:where wind in the upper levels of the 943: 707: 442: 680: 543:Tropical cyclones and climate change 146:circulation and the formation of an 1767:Mediterranean tropical-like cyclone 1760:North Indian Ocean tropical cyclone 1693:Mediterranean tropical-like cyclone 1576:East Asian-northwest Pacific storms 373:Meteorology and Atmospheric Physics 206: 13: 1855:Upper tropospheric cyclonic vortex 1801:Australian region tropical cyclone 321: 128: 14: 2131: 2076: 2062: 1018: 46:), sometimes referred to as the 1815:South Atlantic tropical cyclone 1774:Black Sea tropical-like cyclone 423: 1808:South Pacific tropical cyclone 1571:Continental North Asian storms 411: 399: 360: 306: 292: 280: 268: 256: 1: 249: 2069:Tropical cyclones portal 1110:Great Sheffield Gale of 1962 1050:Moray Firth fishing disaster 593:Ridiculously Resilient Ridge 73: 7: 1919:Mesoscale convective vortex 1901:Mesoscale convective system 1503:List of European windstorms 920:Pacific Northwest windstorm 237: 175:, is therefore uncertain. 157: 10: 2136: 213:Australian east coast lows 201:July 2021 floods in Europe 178: 2056: 2013: 1943: 1934: 1899: 1876: 1867: 1832: 1783: 1721: 1706: 1683:Australian east coast Low 1668: 1639: 1626:Australian east coast low 1618: 1609: 1584: 1553: 1523: 1494: 1224: 1166:1992 New Year's Day Storm 1073: 1027: 1016: 979: 939: 932: 892: 863: 824: 817: 808: 799: 741: 703: 671: 660: 651: 606: 560: 551: 485: 393:10.1007/s00703-006-0220-9 90:. They are formed when a 54:as "a closed upper-level 16:Meteorological phenomenon 2105:Meteorological phenomena 1194:Boxing Day Storm of 1998 1187:Christmas Eve storm 1997 523:Annular tropical cyclone 104:surface weather analysis 52:National Weather Service 1983:Multiple-vortex tornado 1422:Friederike (David) 2018 1415:Eleanor (Burglind) 2018 1138:December 1981 windstorm 1096:North Sea flood of 1953 1009:Christmas Flood of 1717 1924:Line echo wave pattern 1878:Mesoscale ocean eddies 1647:Southern Ocean cyclone 735:Extratropical cyclones 528:Bar (tropical cyclone) 518:Central dense overcast 265:The Earth Observatory 221:extratropical cyclones 192: 138: 35: 1296:Friedhelm/Bawbag 2011 1159:Burns' Day storm 1990 1043:Night of the Big Wind 764:Post-tropical cyclone 513:Rapid intensification 317:Bureau of Meteorology 186: 136: 22: 2120:Atmospheric dynamics 2083:Tornadoes portal 1993:Anticyclonic tornado 1961:Low-topped supercell 1739:Cape Verde hurricane 1131:Gale of January 1976 263:Kona Low over Hawaii 217:subtropical cyclones 144:atmospheric blocking 50:, is defined by the 1785:Southern Hemisphere 1723:Northern Hemisphere 1611:Southern Hemisphere 1566:Western Disturbance 1380:Thomas (Doris) 2017 1152:Great storm of 1987 1117:1968 Scotland storm 1057:Tay Bridge disaster 1036:Great Storm of 1824 1002:Great Storm of 1703 972:European windstorms 801:Northern Hemisphere 619:South Atlantic High 607:Southern Hemisphere 583:North American High 561:Northern Hemisphere 385:2007MAP....96...43L 346:2005JCli...18.3085N 115:Mediterranean Basin 78:A cut-off low is a 1732:Atlantic hurricane 1688:Lake Huron cyclone 749:Anticyclonic storm 624:South Pacific High 588:North Pacific High 503:High-pressure area 493:Anticyclonic storm 354:10.1175/JCLI3386.1 334:Journal of Climate 193: 139: 36: 2092: 2091: 2052: 2051: 2048: 2047: 2044: 2043: 1988:Satellite tornado 1863: 1862: 1828: 1827: 1824: 1823: 1748:Pacific hurricane 1664: 1663: 1660: 1659: 1605: 1604: 1549: 1548: 1519: 1518: 1064:Eyemouth disaster 980:14th-18th century 928: 927: 888: 887: 769:Low-pressure area 647: 646: 639:Subtropical ridge 598:Subtropical ridge 508:Low-pressure area 478:Centers of action 340:(16): 3085–3103. 289:by Weather Online 117:, when a mass of 2127: 2081: 2080: 2079: 2067: 2066: 2065: 1941: 1940: 1874: 1873: 1817: 1810: 1803: 1796: 1786: 1776: 1769: 1762: 1750: 1741: 1734: 1724: 1719: 1718: 1631:Black nor'easter 1616: 1615: 1612: 1531:Black Sea storms 1512: 1505: 1487: 1480: 1473: 1466: 1459: 1452: 1445: 1438: 1431: 1424: 1417: 1410: 1403: 1396: 1389: 1382: 1375: 1368: 1361: 1354: 1347: 1340: 1333: 1326: 1319: 1312: 1305: 1298: 1291: 1284: 1277: 1270: 1263: 1256: 1249: 1242: 1235: 1217: 1210: 1203: 1196: 1189: 1182: 1175: 1173:Braer Storm 1993 1168: 1161: 1154: 1147: 1140: 1133: 1126: 1119: 1112: 1105: 1098: 1091: 1084: 1066: 1059: 1052: 1045: 1038: 1022: 1011: 1004: 997: 990: 974: 964: 957: 950: 941: 940: 937: 936: 881: 874: 856: 849: 842: 835: 822: 821: 815: 814: 811: 806: 805: 802: 728: 721: 714: 705: 704: 678: 677: 674: 669: 668: 665: 658: 657: 614:South Polar High 568:North Polar High 558: 557: 463: 456: 449: 440: 439: 433: 427: 421: 415: 409: 403: 397: 396: 364: 358: 357: 325: 319: 310: 304: 303: 296: 290: 284: 278: 272: 266: 260: 207:Regional impacts 173:weather blockage 60:westerly current 48:weatherman's woe 2135: 2134: 2130: 2129: 2128: 2126: 2125: 2124: 2095: 2094: 2093: 2088: 2077: 2075: 2063: 2061: 2040: 2009: 1930: 1895: 1859: 1820: 1813: 1806: 1799: 1792: 1784: 1779: 1772: 1765: 1758: 1746: 1737: 1730: 1722: 1710: 1702: 1656: 1635: 1610: 1601: 1580: 1545: 1515: 1508: 1501: 1490: 1483: 1476: 1469: 1462: 1455: 1448: 1441: 1434: 1427: 1420: 1413: 1406: 1399: 1392: 1385: 1378: 1371: 1364: 1357: 1350: 1343: 1336: 1329: 1322: 1315: 1308: 1301: 1294: 1287: 1280: 1273: 1266: 1259: 1252: 1245: 1238: 1231: 1220: 1213: 1206: 1199: 1192: 1185: 1178: 1171: 1164: 1157: 1150: 1143: 1136: 1129: 1122: 1115: 1108: 1101: 1094: 1087: 1080: 1069: 1062: 1055: 1048: 1041: 1034: 1023: 1014: 1007: 1000: 995:Burchardi flood 993: 988:Grote Mandrenke 986: 975: 970: 968: 924: 884: 877: 870: 859: 852: 847:Great basin low 845: 838: 833:Alberta clipper 831: 809: 800: 795: 737: 732: 699: 695:South Polar low 690:North Polar low 672: 661: 643: 634:Australian High 602: 547: 481: 467: 437: 436: 428: 424: 416: 412: 404: 400: 365: 361: 326: 322: 311: 307: 298: 297: 293: 285: 281: 273: 269: 261: 257: 252: 240: 209: 181: 160: 148:upper level low 131: 129:Characteristics 100:core of the low 76: 17: 12: 11: 5: 2133: 2123: 2122: 2117: 2115:Weather events 2112: 2107: 2090: 2089: 2087: 2086: 2072: 2057: 2054: 2053: 2050: 2049: 2046: 2045: 2042: 2041: 2039: 2038: 2033: 2028: 2023: 2017: 2015: 2011: 2010: 2008: 2007: 2002: 1997: 1996: 1995: 1990: 1985: 1975: 1970: 1969: 1968: 1963: 1958: 1947: 1945: 1938: 1932: 1931: 1929: 1928: 1927: 1926: 1916: 1911: 1905: 1903: 1897: 1896: 1894: 1893: 1888: 1882: 1880: 1871: 1865: 1864: 1861: 1860: 1858: 1857: 1852: 1847: 1842: 1836: 1834: 1830: 1829: 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1068: 1067: 1060: 1053: 1046: 1039: 1031: 1029: 1025: 1024: 1017: 1015: 1013: 1012: 1005: 998: 991: 983: 981: 977: 976: 967: 966: 959: 952: 944: 934: 930: 929: 926: 925: 923: 922: 917: 912: 907: 902: 896: 894: 890: 889: 886: 885: 883: 882: 875: 872:Panhandle hook 867: 865: 861: 860: 858: 857: 850: 843: 836: 828: 826: 819: 812: 803: 797: 796: 794: 793: 788: 787: 786: 776: 771: 766: 761: 756: 751: 745: 743: 739: 738: 731: 730: 723: 716: 708: 701: 700: 698: 697: 692: 686: 684: 675: 666: 663:Synoptic scale 655: 649: 648: 645: 644: 642: 641: 636: 631: 626: 621: 616: 610: 608: 604: 603: 601: 600: 595: 590: 585: 580: 575: 570: 564: 562: 555: 549: 548: 546: 545: 540: 535: 530: 525: 520: 515: 510: 505: 500: 495: 489: 487: 483: 482: 476:of the world ( 466: 465: 458: 451: 443: 435: 434: 422: 410: 398: 379:(1–2): 43–60. 359: 320: 305: 291: 279: 267: 254: 253: 251: 248: 247: 246: 239: 236: 208: 205: 180: 177: 159: 156: 130: 127: 75: 72: 15: 9: 6: 4: 3: 2: 2132: 2121: 2118: 2116: 2113: 2111: 2108: 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1572: 1569: 1567: 1564: 1562: 1559: 1558: 1556: 1552: 1542: 1539: 1537: 1536:Icelandic Low 1534: 1532: 1529: 1528: 1526: 1522: 1511: 1507: 1504: 1500: 1499: 1497: 1493: 1486: 1482: 1479: 1475: 1472: 1468: 1465: 1461: 1458: 1454: 1451: 1447: 1444: 1440: 1437: 1433: 1430: 1426: 1423: 1419: 1416: 1412: 1409: 1405: 1402: 1398: 1395: 1391: 1388: 1384: 1381: 1377: 1374: 1370: 1367: 1363: 1360: 1356: 1353: 1349: 1346: 1342: 1339: 1335: 1332: 1328: 1325: 1321: 1318: 1314: 1311: 1307: 1304: 1300: 1297: 1293: 1290: 1286: 1283: 1279: 1276: 1272: 1269: 1265: 1262: 1258: 1255: 1251: 1248: 1244: 1241: 1237: 1234: 1230: 1229: 1227: 1223: 1216: 1212: 1209: 1205: 1202: 1198: 1195: 1191: 1188: 1184: 1181: 1177: 1174: 1170: 1167: 1163: 1160: 1156: 1153: 1149: 1146: 1142: 1139: 1135: 1132: 1128: 1125: 1121: 1118: 1114: 1111: 1107: 1104: 1100: 1097: 1093: 1090: 1086: 1083: 1079: 1078: 1076: 1072: 1065: 1061: 1058: 1054: 1051: 1047: 1044: 1040: 1037: 1033: 1032: 1030: 1026: 1021: 1010: 1006: 1003: 999: 996: 992: 989: 985: 984: 982: 978: 973: 965: 960: 958: 953: 951: 946: 945: 942: 938: 935: 931: 921: 918: 916: 913: 911: 908: 906: 903: 901: 898: 897: 895: 891: 880: 879:November gale 876: 873: 869: 868: 866: 862: 855: 851: 848: 844: 841: 837: 834: 830: 829: 827: 823: 820: 816: 813: 810:North America 807: 804: 798: 792: 789: 785: 782: 781: 780: 777: 775: 772: 770: 767: 765: 762: 760: 757: 755: 752: 750: 747: 746: 744: 740: 736: 729: 724: 722: 717: 715: 710: 709: 706: 702: 696: 693: 691: 688: 687: 685: 683: 679: 676: 673:Surface-based 670: 667: 664: 659: 656: 654: 650: 640: 637: 635: 632: 630: 629:Kalahari High 627: 625: 622: 620: 617: 615: 612: 611: 609: 605: 599: 596: 594: 591: 589: 586: 584: 581: 579: 576: 574: 573:Siberian High 571: 569: 566: 565: 563: 559: 556: 554: 550: 544: 541: 539: 536: 534: 531: 529: 526: 524: 521: 519: 516: 514: 511: 509: 506: 504: 501: 499: 496: 494: 491: 490: 488: 484: 479: 475: 471: 464: 459: 457: 452: 450: 445: 444: 441: 431: 426: 419: 414: 407: 402: 394: 390: 386: 382: 378: 374: 370: 363: 355: 351: 347: 343: 339: 335: 331: 324: 318: 314: 309: 301: 295: 288: 283: 276: 271: 264: 259: 255: 245: 244:Cold-core low 242: 241: 235: 233: 228: 226: 222: 218: 214: 204: 202: 198: 197:thunderstorms 190: 185: 176: 174: 169: 165: 155: 153: 149: 145: 135: 126: 124: 120: 116: 111: 109: 105: 101: 97: 93: 89: 85: 81: 80:cold-core low 71: 69: 65: 61: 57: 53: 49: 45: 41: 33: 29: 25: 21: 2074: 2060: 1973:Funnel cloud 1891:Haida Eddies 1850:Polar vortex 1844: 1408:Herwart 2017 1401:Ophelia 2017 1324:St Jude 2013 1303:Joachim 2011 1282:Xynthia 2010 1240:Jeanett 2002 1225:21st century 1145:Charley 1986 1082:Ulysses 1903 1074:20th century 1028:19th century 905:Hatteras low 900:Aleutian Low 840:Colorado low 774:Weather bomb 474:anticyclones 425: 413: 401: 376: 372: 362: 337: 333: 323: 313:Cut-off Lows 308: 294: 282: 270: 258: 229: 215:, which are 210: 194: 161: 140: 112: 77: 47: 43: 39: 37: 2031:Steam devil 1951:Mesocyclone 1845:Cut-off low 1833:Upper level 1670:Subtropical 1640:Other areas 1585:Other areas 1561:Asiatic Low 1485:Ciarán 2023 1471:Larisa 2023 1464:Eunice 2022 1450:Aurore 2021 1443:Dennis 2020 1429:Adrian 2018 1394:Xavier 2017 1366:Niklas 2015 1317:Andrea 2012 1310:Dagmar 2011 1261:Kyrill 2007 1247:Gudrun 2005 1233:Oratia 2000 1215:Martin 1999 1208:Lothar 1999 1201:Anatol 1999 1103:Debbie 1961 1089:Iberia 1941 854:Bighorn Low 825:Lee Cyclone 818:Continental 578:Azores High 553:Anticyclone 287:Cut-off low 168:convergence 98:around the 84:troposphere 40:cut-off low 2099:Categories 2036:Fire whirl 2026:Dust devil 2005:Waterspout 1966:Wall cloud 1678:Kona storm 1597:Kona storm 1478:Babet 2023 1457:Malik 2022 1436:Ciara 2020 1331:Xaver 2013 1289:Berit 2011 1275:Klaus 2009 910:Nor'easter 533:Superstorm 250:References 225:subtropics 164:baroclinic 88:jet stream 70:for days. 68:stationary 64:subtropics 44:cutoff low 32:jet stream 2000:Landspout 1956:Supercell 1936:Whirlwind 1869:Mesoscale 1652:Sudestada 1619:Australia 1541:Genoa low 1387:Zeus 2017 1373:Egon 2017 1359:Tini 2014 1345:Anne 2014 1338:Dirk 2013 1268:Emma 2008 1180:Lili 1996 779:Sting jet 538:Hypercane 420:EUMeTrain 408:EUMeTrain 232:cold drop 152:sea level 119:polar air 96:isotherms 74:Formation 2021:Gustnado 1914:Mesohigh 1909:Wake Low 1708:Tropical 1495:See also 1254:Per 2007 915:Gulf low 791:Rainband 742:Concepts 486:Concepts 470:Cyclones 238:See also 189:Alicante 158:Movement 123:altitude 24:Kona Low 1978:Tornado 1754:Typhoon 1713:Outline 1698:Thermal 893:Oceanic 759:Cyclone 653:Cyclone 381:Bibcode 342:Bibcode 315:by the 277:WUSA-TV 179:Effects 1592:Arctic 933:Europe 92:trough 28:Hawaii 2014:Minor 1944:Major 1524:Other 864:Other 754:Storm 682:Polar 498:Storm 108:block 26:over 2110:Cold 1554:Asia 784:List 472:and 42:(or 389:doi 350:doi 234:". 219:or 56:low 2101:: 387:. 377:96 375:. 371:. 348:. 338:18 336:. 332:. 227:. 203:. 154:. 125:. 38:A 1715:) 1711:( 963:e 956:t 949:v 727:e 720:t 713:v 480:) 462:e 455:t 448:v 395:. 391:: 383:: 356:. 352:: 344:: 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Index


Kona Low
Hawaii
jet stream
National Weather Service
low
westerly current
subtropics
stationary
cold-core low
troposphere
jet stream
trough
isotherms
core of the low
surface weather analysis
block
Mediterranean Basin
polar air
altitude

atmospheric blocking
upper level low
sea level
baroclinic
convergence
weather blockage

Alicante
thunderstorms

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