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Western disturbance

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133: 260: 360:... The onset of a western disturbance is heralded by dense thunder clouds accompanied by heavy rain or snow. The weather conditions during winter are generally influenced by the distribution pattern of pressure in Central and West Asia. In winter, due to the shifting of the pressure belts, the westerlies blow from 20°N to 50°N latitude and Northern India comes under the influence of the winds and cyclones rising from the Mediterranean Sea. In the wake of the disturbance comes cold air and often accompanied by strong winds ... 243: 36: 952: 268:
winter season has great importance in agriculture, particularly for the rabi crops. Wheat among them is one of the most important crops, which helps to meet India's food security. An average of four to five western disturbances form during the winter season. The rainfall distribution and amount varies with every western disturbance.
544:... These states are: Punjab, Haryana, Himachal Pradesh, Jammu & Kashmir, Uttarakhand and Uttar Pradesh. These states receive some rainfall (precipitation) during the rabi season, brought about by western disturbances, which originate in the Mediterranean region. These showers are very beneficial for rabi crops ... 300:
current generally progresses from east to west in the northern Himalayan region, unlike western disturbances which follow a west to east trend in north India with consequent rise in pressure carrying cold pool of air. This helps in the activation of monsoon in Pakistan and certain parts of northwest
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Western disturbances, specifically the ones in winter, bring moderate to heavy rain in low-lying areas and heavy snow to mountainous areas of the Indian Subcontinent. They are the cause of most winter and post-monsoon season rainfall across Pakistan and northwest India. Precipitation during the
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Western disturbances noticed as cyclonic circulation/trough in the mid and lower tropospheric levels or as a low-pressure area on the surface, which occur in middle latitude westerlies and originate over the Mediterranean Sea, Caspian Sea and Black Sea and move eastwards across north
235:. Traveling at speeds up to 12 m/s (43 km/h; 27 mph), the disturbance moves towards the Indian subcontinent until the Himalayas inhibits its development, upon which the depression rapidly weakens. The western disturbances are embedded in the mid-latitude 392:... Rains during winter mont in north India are due to occurrence of low pressure system called western disturbances. This moves from the west to the east causing snow fall in the high ranges in the Himalayas and rains in sub-mountainous tracts and adjoining areas ... 280:
conditions and dense fog. These conditions remain stable until disturbed by another western disturbance. When western disturbances move across northwest India before the onset of monsoon, a temporary advancement of monsoon current appears over the region.
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Western disturbances are usually associated with cloudy sky, higher night temperatures and unusual rain. Excessive precipitation due to western disturbances can cause crop damage, landslides, floods and avalanches. Over the
566:... In northern India rainfall occurs again during the year in connection with the Western Disturbances which are of great agricultural importance to north-west India as they occur chiefly during the Rabi ... 263:
A strong western disturbance affecting the northern parts of the Indian subcontinent in February 2013. Such disturbances bring substantial amount of rainfall and are a threat to lives and property.
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where the moisture is carried in the lower atmosphere. In the case of the Indian subcontinent, moisture is sometimes shed as rain when the storm system encounters the
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Western disturbances start declining in numbers after winter. During the summer months of April and May, they move across north India. The
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A western disturbance moving east towards the Indian subcontinent. It can be seen as a cloud patch originating from the
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Dimri, A. P.; Niyogi, D.; Barros, A. P.; Ridley, J.; Mohanty, U. C.; Yasunari, T.; Sikka, D. R. (June 2015).
1618: 1523: 1097: 981: 879: 312:, which killed more than 5000 people in a span of 3 days, is said to be a result of one such interaction. 1434: 851: 919: 715: 1623: 1557: 223:
towards an area of relatively warmer air with high moisture. This generates favorable conditions for
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with western disturbances may occasionally cause dense clouding and heavy precipitation. The
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India. It also causes pre-monsoon rainfall especially in northern India.
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and neighbourhood consolidates, causing the intrusion of cold air from
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A Western Disturbance over Northern India and Pakistan in November 2012
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Hunt, Kieran M. R.; Turner, Andrew G.; Shaffrey, Len C. (2017-11-11).
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The strongest western disturbances usually occur in the western and
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that brings sudden winter rain to the northwestern parts of the
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Western disturbances originate in the Mediterranean region. A
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Western disturbances are important for the development of the
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in the upper atmosphere, which promotes the formation of an
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Savage Planet: Storms of the Century – Extratropical Storms
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Western Disturbances – An Indian Meteorological Perspective
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Social Science (A Textbook in Geography Part II) Class X
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Quarterly Journal of the Royal Meteorological Society
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Irrigation water management: principles and practice
623:PBS Savage Planet feature on extratropical storms, 156:, which extends as east as up to northern parts of 60:. Unsourced material may be challenged and removed. 496: 463:Dimri, A.P.; Chevuturi, Amulya (9 February 2016). 1600: 431:Experimental Agrometeorology: A Practical Manual 1442:List of atmospheric pressure records in Europe 462: 372: 199:, which includes the locally important staple 887: 651: 631:Extratropical storms are major weather makers 423: 531: 529: 629:USA Today article on extratropical storms, 894: 880: 665: 658: 644: 254: 604: 557:J.E. Parkinson, R. H. Whitehouse (1927). 550: 526: 517: 458: 456: 454: 452: 366: 120:Learn how and when to remove this message 258: 241: 131: 901: 334: 14: 1601: 449: 404: 875: 639: 291: 563:. 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Springer. pp. 5, 6, 7. 398: 347:, India International Centre, 250:, progressing east thereafter. 13: 1: 405:Faridi, Rashid (2013-02-24). 327: 1042:Great Sheffield Gale of 1962 982:Moray Firth fishing disaster 206: 7: 1435:List of European windstorms 852:Pacific Northwest windstorm 315: 10: 1640: 286:northern parts of Pakistan 276:, they occasionally bring 1571: 1558:Australian east coast low 1550: 1541: 1516: 1485: 1455: 1426: 1156: 1098:1992 New Year's Day Storm 1005: 959: 948: 911: 871: 864: 824: 795: 756: 749: 740: 731: 673: 379:. PHI Learning Pvt. Ltd. 1614:Regional climate effects 1126:Boxing Day Storm of 1998 1119:Christmas Eve storm 1997 233:extratropical depression 1354:Friederike (David) 2018 1347:Eleanor (Burglind) 2018 1070:December 1981 windstorm 1028:North Sea flood of 1953 941:Christmas Flood of 1717 373:D. K. Majumdar (2004). 310:2013 North India floods 255:Significance and impact 1579:Southern Ocean cyclone 667:Extratropical cyclones 264: 251: 137: 1228:Friedhelm/Bawbag 2011 1091:Burns' Day storm 1990 975:Night of the Big Wind 696:Post-tropical cyclone 585:Reviews of Geophysics 262: 245: 186:tropical counterparts 135: 69:"Western disturbance" 1063:Gale of January 1976 606:10.1002/2014RG000460 274:Indo-Gangetic plains 150:Mediterranean region 54:improve this article 1619:Climate of Pakistan 1543:Southern Hemisphere 1498:Western Disturbance 1312:Thomas (Doris) 2017 1084:Great storm of 1987 1049:1968 Scotland storm 989:Tay Bridge disaster 968:Great Storm of 1824 934:Great Storm of 1703 904:European windstorms 733:Northern Hemisphere 597:2015RvGeo..53..225D 541:. FK Publications. 154:Indian subcontinent 148:originating in the 146:extratropical storm 142:western disturbance 18:Western Disturbance 681:Anticyclonic storm 292:Effects on monsoon 265: 252: 213:high-pressure area 160:and South eastern 138: 1596: 1595: 1592: 1591: 1537: 1536: 1481: 1480: 1451: 1450: 996:Eyemouth disaster 912:14th-18th century 860: 859: 820: 819: 701:Low-pressure area 386:978-81-203-1729-1 354:978-0-19-561254-7 322:Tropical cyclones 298:southwest monsoon 174:Mediterranean Sea 130: 129: 122: 104: 16:(Redirected from 1631: 1624:Climate of India 1563:Black nor'easter 1548: 1547: 1544: 1463:Black Sea storms 1444: 1437: 1419: 1412: 1405: 1398: 1391: 1384: 1377: 1370: 1363: 1356: 1349: 1342: 1335: 1328: 1321: 1314: 1307: 1300: 1293: 1286: 1279: 1272: 1265: 1258: 1251: 1244: 1237: 1230: 1223: 1216: 1209: 1202: 1195: 1188: 1181: 1174: 1167: 1149: 1142: 1135: 1128: 1121: 1114: 1107: 1105:Braer Storm 1993 1100: 1093: 1086: 1079: 1072: 1065: 1058: 1051: 1044: 1037: 1030: 1023: 1016: 998: 991: 984: 977: 970: 954: 943: 936: 929: 922: 906: 896: 889: 882: 873: 872: 869: 868: 813: 806: 788: 781: 774: 767: 754: 753: 747: 746: 743: 738: 737: 734: 660: 653: 646: 637: 636: 611: 610: 608: 576: 570: 569: 554: 548: 547: 533: 524: 523: 521: 512:(710): 278–290. 503: 494: 488: 487: 485: 483: 460: 447: 427: 421: 420: 418: 417: 402: 396: 395: 370: 364: 363: 338: 125: 118: 114: 111: 105: 103: 62: 38: 30: 21: 1639: 1638: 1634: 1633: 1632: 1630: 1629: 1628: 1599: 1598: 1597: 1588: 1567: 1542: 1533: 1512: 1477: 1447: 1440: 1433: 1422: 1415: 1408: 1401: 1394: 1387: 1380: 1373: 1366: 1359: 1352: 1345: 1338: 1331: 1324: 1317: 1310: 1303: 1296: 1289: 1282: 1275: 1268: 1261: 1254: 1247: 1240: 1233: 1226: 1219: 1212: 1205: 1198: 1191: 1184: 1177: 1170: 1163: 1152: 1145: 1138: 1131: 1124: 1117: 1110: 1103: 1096: 1089: 1082: 1075: 1068: 1061: 1054: 1047: 1040: 1033: 1026: 1019: 1012: 1001: 994: 987: 980: 973: 966: 955: 946: 939: 932: 927:Burchardi flood 925: 920:Grote Mandrenke 918: 907: 902: 900: 856: 816: 809: 802: 791: 784: 779:Great basin low 777: 770: 765:Alberta clipper 763: 741: 732: 727: 669: 664: 620: 615: 614: 577: 573: 555: 551: 535: 534: 527: 519:10.1002/qj.3200 501: 495: 491: 481: 479: 477: 461: 450: 428: 424: 415: 413: 403: 399: 387: 371: 367: 355: 339: 335: 330: 318: 294: 257: 209: 126: 115: 109: 106: 63: 61: 51: 39: 28: 23: 22: 15: 12: 11: 5: 1637: 1627: 1626: 1621: 1616: 1611: 1594: 1593: 1590: 1589: 1587: 1586: 1581: 1575: 1573: 1569: 1568: 1566: 1565: 1560: 1554: 1552: 1545: 1539: 1538: 1535: 1534: 1532: 1531: 1526: 1520: 1518: 1514: 1513: 1511: 1510: 1505: 1500: 1495: 1489: 1487: 1483: 1482: 1479: 1478: 1476: 1475: 1470: 1465: 1459: 1457: 1453: 1452: 1449: 1448: 1446: 1445: 1438: 1430: 1428: 1424: 1423: 1421: 1420: 1413: 1406: 1399: 1392: 1385: 1378: 1371: 1364: 1357: 1350: 1343: 1336: 1329: 1322: 1315: 1308: 1301: 1294: 1287: 1284:Christina 2014 1280: 1273: 1266: 1259: 1252: 1245: 1238: 1231: 1224: 1217: 1210: 1203: 1196: 1189: 1182: 1175: 1168: 1160: 1158: 1154: 1153: 1151: 1150: 1143: 1136: 1129: 1122: 1115: 1108: 1101: 1094: 1087: 1080: 1073: 1066: 1059: 1056:Quimburga 1972 1052: 1045: 1038: 1031: 1024: 1017: 1009: 1007: 1003: 1002: 1000: 999: 992: 985: 978: 971: 963: 961: 957: 956: 949: 947: 945: 944: 937: 930: 923: 915: 913: 909: 908: 899: 898: 891: 884: 876: 866: 862: 861: 858: 857: 855: 854: 849: 844: 839: 834: 828: 826: 822: 821: 818: 817: 815: 814: 807: 804:Panhandle hook 799: 797: 793: 792: 790: 789: 782: 775: 768: 760: 758: 751: 744: 735: 729: 728: 726: 725: 720: 719: 718: 708: 703: 698: 693: 688: 683: 677: 675: 671: 670: 663: 662: 655: 648: 640: 634: 633: 627: 619: 618:External links 616: 613: 612: 591:(2): 225–246. 571: 549: 525: 489: 476:978-3319267371 475: 448: 422: 397: 385: 365: 353: 332: 331: 329: 326: 325: 324: 317: 314: 293: 290: 256: 253: 208: 205: 164:. 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Index

Western Disturbance

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extratropical storm
Mediterranean region
Indian subcontinent
Bangladesh
Nepal
monsoonal
westerlies
Mediterranean Sea
Caspian Sea
Black Sea
tropical counterparts
Himalayas
Rabi crop
wheat
high-pressure area
Ukraine
polar regions

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