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Central American gyre

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105: 2372: 22: 2386: 120:. However, the emergence of northwesterly winds over Central America can lead to the development of a CAG as the climatological wind pattern is interrputed. CAGs arise more frequently in the fall than the spring when the easterly trade winds are more relaxed, with the frequency of CAGs maximized in October. This interruption of the climatological trade winds tends to occur more frequently during certain phases of the 1328: 199:. This occurs about once every other year on average, and tropical cyclone development occurs in tandem with around half of all CAGs. Tropical cyclogenesis typically occurs on the northeastern periphery of the gyre, with the resulting tropical cyclone tracking counterclockwise along with the flow about the gyre. 84:. The terrain of Central America may influence the development and organization of the showers and thunderstorms associated with CAGs. On average, precipitation associated with CAGs most commonly occurs along the coast of Central America. 214:
winds are higher, the tropical cyclones associated with CAGs tend to be weaker than those occurring during the peak of the hurricane season. However, suitable conditions can facilitate the development of stronger storms; for example,
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after forming in association with a CAG. CAGs can also help produce tropical cyclones in the eastern Pacific and western Atlantic simultaneously. In May and June 2020, a CAG contributed to the formation of
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and persistently generate inclement weather. Consequently, with the aid of the nearby ocean waters, CAGs can produce prolific amounts of rainfall over Central America, presenting a risk for
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in the upper-troposphere atop the gyre. This class of CAGs is associated with enhanced moisture and precipitation around the center of the gyre. Less frequently, a CAG may exhibit a
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Lamers, Alex; Devi. S, Sunitha; Sharma, Monica; Berg, Robbie; Gálvez, José Manuel; Yu, Zifeng; Kriat, Tarik; Cardos, Sareti; Grant, David; Moron, Lorenzo A. (June 2023).
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may also contribute to the evolution of CAGs. The rarity of CAGs during the summer is associated with the concurrent lack of northwesterly flow over the
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are more abundant over Central America. The weakening of easterlies can produce cyclonic flow over Central America and enable CAG formation. Localized
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in the upper-troposphere. The regions of anomalous moisture and precipitation associated with these CAGs are concentrated east of the gyre's center.
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of winds associated with CAGs is weak. CAGs may span across hundreds of miles, potentially covering parts of the eastern Pacific Ocean, southern
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CAGs consist of smaller vortices that rotate about the broader gyre. These localized areas of low pressure are associated with stronger
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between May and November, and most commonly occurs during late spring (May–June) and early fall (October–November). CAGs are a type of
2162: 2108: 768: 487: 1262: 518: 2122: 2081: 1019: 658:"A Tropical Depression or Storm May Form in the Caribbean Sea or Gulf of Mexico From a 'Central American Gyre' By This Weekend" 2115: 121: 2417: 2412: 1883: 148:. One analysis identified 47 CAGs occurring between 1980 and 2010, corresponding to roughly 1.5 CAGs per year. 2020: 1899: 1473: 1357: 1255: 900: 233: 232:
in the eastern Pacific and Gulf of Mexico. The complex weather patterns associated with CAGs presents difficulties for
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the development of tropical cyclones in the western Caribbean in part due to the complexities associated with CAGs.
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and can generate pockets of higher vorticity. They often result from the interaction between the gyre and a passing
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from a nearby CAG, enhancing the amount of rainfall they produce. The presence of a CAG may also push
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CAGs are broad circulations and present risks for flash floods and mudslides over Central America.
2039: 1279: 1161: 1056: 931: 895: 810: 800: 192: 89: 519:"Central American Gyre Could Trigger Dangerous Flooding, But Not Caribbean Tropical Development" 2295: 2055: 1659: 1431: 1371: 1076: 946: 905: 815: 785: 754: 216: 188: 62: 46: 30: 2390: 2015: 1603: 730: 605: 564: 343: 184: 141: 85: 26: 1715: 1610: 1589: 1547: 1302: 1140: 941: 113: 73: 1792: 726: 601: 560: 339: 2268: 1673: 1631: 1624: 1617: 1568: 1554: 1540: 1515: 1508: 1179: 145: 137: 72:
CAGs are also slow-moving and can last on the order of days to weeks as they move over
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and share similarities with monsoonal lows in other oceanic basins. The broad
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Papin, Philippe P.; Bosart, Lance F.; Torn, Ryan D. (1 May 2017).
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produced by breaks in the Central American terrain such as the
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over the western Caribbean Sea and southern Gulf of Mexico may
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and detach from the gyre if the environment is conducive to
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in the southern Gulf of Mexico towards the south and west.
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Due to the prevalence of CAGs either early or late in the
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across the tropical eastern Pacific and Atlantic tend to
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that occurs over the eastern Pacific Ocean and western
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The 2248: 2181: 2026: 1923: 1270: 1256: 1248: 1244: 1129: 1122: 1113: 1034: 1020: 1012: 985: 976: 965: 865: 769: 755: 747: 488:"Central America faces major flood threat" 94:rainfall associated with tropical cyclones 734: 609: 568: 347: 324:"A Climatology of Central American Gyres" 2102:South-West Indian Ocean tropical cyclone 257: 155:structure, occurring in tandem with an 16:Broad rainy season low-pressure system 163:structure and occur in tandem with a 7: 851:Tropical cyclones and climate change 715:Tropical Cyclone Research and Review 684:"Cristobal Drenches Central America" 230:Tropical storms Amanda and Cristobal 2075:Mediterranean tropical-like cyclone 2068:North Indian Ocean tropical cyclone 2001:Mediterranean tropical-like cyclone 1884:East Asian-northwest Pacific storms 656:Belles, Jonathan (2 October 2017). 410:Sosnowski, Alex (16 October 2020). 25:Central American gyres can produce 2163:Upper tropospheric cyclonic vortex 2109:Australian region tropical cyclone 628:Papin, Philippe (9 October 2018). 467:. Laredo, Texas: Hearst Newspapers 459:Bradshaw, Robin (29 August 2023). 280:"What is a Central American Gyre?" 183:. A vortex may consolidate into a 171:Influence on tropical cyclogenesis 14: 2384: 2370: 1326: 517:Erdman, Jonathan (19 May 2022). 433:Sonowski, Alex (15 June 2023) . 278:Wulfeck, Andrew (10 June 2023). 2123:South Atlantic tropical cyclone 2082:Black Sea tropical-like cyclone 2116:South Pacific tropical cyclone 1879:Continental North Asian storms 549:GIScience & Remote Sensing 486:Van Dam, Derek (30 May 2020). 1: 682:Voiland, Adam (5 June 2020). 570:10.1080/15481603.2021.1908675 69:, and western Caribbean Sea. 2377:Tropical cyclones portal 1418:Great Sheffield Gale of 1962 1358:Moray Firth fishing disaster 901:Ridiculously Resilient Ridge 197:tropical cyclone development 63:counterclockwise circulation 2227:Mesoscale convective vortex 2209:Mesoscale convective system 1811:List of European windstorms 1228:Pacific Northwest windstorm 372:Henson, Bob (29 May 2020). 2439: 736:10.1016/j.tcrr.2023.06.005 45:) is a broad and seasonal 2364: 1991:Australian east coast Low 1934:Australian east coast low 1474:1992 New Year's Day Storm 1324: 1247: 1011: 122:Madden–Julian oscillation 100:Development and structure 1502:Boxing Day Storm of 1998 1495:Christmas Eve storm 1997 831:Annular tropical cyclone 611:10.1175/JAMC-D-18-0034.1 208:sea surface temperatures 2291:Multiple-vortex tornado 1730:Friederike (David) 2018 1723:Eleanor (Burglind) 2018 1446:December 1981 windstorm 1404:North Sea flood of 1953 1317:Christmas Flood of 1717 349:10.1175/MWR-D-16-0411.1 2232:Line echo wave pattern 2186:Mesoscale ocean eddies 1955:Southern Ocean cyclone 1043:Extratropical cyclones 836:Bar (tropical cyclone) 826:Central dense overcast 328:Monthly Weather Review 238:Global Forecast System 109: 34: 1604:Friedhelm/Bawbag 2011 1467:Burns' Day storm 1990 1351:Night of the Big Wind 1072:Post-tropical cyclone 821:Rapid intensification 380:. Weather Underground 107: 39:Central American gyre 24: 2418:Atmospheric dynamics 2413:Tropical meteorology 2391:Tornadoes portal 2301:Anticyclonic tornado 2269:Low-topped supercell 2047:Cape Verde hurricane 1439:Gale of January 1976 225:Category 5 hurricane 210:are lower and upper- 151:Most CAGs exhibit a 47:area of low pressure 2093:Southern Hemisphere 2031:Northern Hemisphere 1919:Southern Hemisphere 1874:Western Disturbance 1688:Thomas (Doris) 2017 1460:Great storm of 1987 1425:1968 Scotland storm 1365:Tay Bridge disaster 1344:Great Storm of 1824 1310:Great Storm of 1703 1280:European windstorms 1109:Northern Hemisphere 927:South Atlantic High 915:Southern Hemisphere 891:North American High 869:Northern Hemisphere 727:2023TCRR...12..100L 662:The Weather Channel 636:The Washington Post 602:2018JApMC..57.1711Z 561:2021GISRS..58..542Z 523:The Weather Channel 340:2017MWRv..145.1983P 2040:Atlantic hurricane 1996:Lake Huron cyclone 1057:Anticyclonic storm 932:South Pacific High 896:North Pacific High 811:High-pressure area 801:Anticyclonic storm 286:. FOX News Network 246:erroneously depict 118:blow from the east 110: 35: 2400: 2399: 2360: 2359: 2356: 2355: 2352: 2351: 2296:Satellite tornado 2171: 2170: 2136: 2135: 2132: 2131: 2056:Pacific hurricane 1972: 1971: 1968: 1967: 1913: 1912: 1857: 1856: 1827: 1826: 1372:Eyemouth disaster 1288:14th-18th century 1236: 1235: 1196: 1195: 1077:Low-pressure area 955: 954: 947:Subtropical ridge 906:Subtropical ridge 816:Low-pressure area 786:Centers of action 688:Earth Observatory 217:Hurricane Michael 86:Tropical cyclones 31:Hurricane Michael 27:tropical cyclones 2430: 2423:Types of cyclone 2389: 2388: 2387: 2375: 2374: 2373: 2249: 2182: 2125: 2118: 2111: 2104: 2094: 2084: 2077: 2070: 2058: 2049: 2042: 2032: 2027: 1939:Black nor'easter 1924: 1920: 1839:Black Sea storms 1820: 1813: 1795: 1788: 1781: 1774: 1767: 1760: 1753: 1746: 1739: 1732: 1725: 1718: 1711: 1704: 1697: 1690: 1683: 1676: 1669: 1662: 1655: 1648: 1641: 1634: 1627: 1620: 1613: 1606: 1599: 1592: 1585: 1578: 1571: 1564: 1557: 1550: 1543: 1525: 1518: 1511: 1504: 1497: 1490: 1483: 1481:Braer Storm 1993 1476: 1469: 1462: 1455: 1448: 1441: 1434: 1427: 1420: 1413: 1406: 1399: 1392: 1374: 1367: 1360: 1353: 1346: 1330: 1319: 1312: 1305: 1298: 1282: 1272: 1265: 1258: 1249: 1245: 1189: 1182: 1164: 1157: 1150: 1143: 1130: 1123: 1119: 1114: 1110: 1036: 1029: 1022: 1013: 986: 982: 977: 973: 966: 922:South Polar High 876:North Polar High 866: 771: 764: 757: 748: 741: 740: 738: 706: 700: 699: 697: 695: 679: 673: 672: 670: 668: 653: 647: 646: 644: 642: 633: 625: 616: 615: 613: 596:(8): 1711–1727. 581: 575: 574: 572: 540: 534: 533: 531: 529: 514: 503: 502: 500: 498: 483: 477: 476: 474: 472: 456: 447: 446: 444: 442: 430: 424: 423: 421: 419: 407: 390: 389: 387: 385: 369: 354: 353: 351: 334:(5): 1983–2000. 319: 296: 295: 293: 291: 275: 240:operated by the 204:hurricane season 193:western Atlantic 185:tropical cyclone 142:Gulf of Papagayo 114:prevailing winds 2438: 2437: 2433: 2432: 2431: 2429: 2428: 2427: 2403: 2402: 2401: 2396: 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1215: 1210: 1204: 1202: 1198: 1197: 1194: 1193: 1191: 1190: 1183: 1180:Panhandle hook 1175: 1173: 1169: 1168: 1166: 1165: 1158: 1151: 1144: 1136: 1134: 1127: 1120: 1111: 1105: 1104: 1102: 1101: 1096: 1095: 1094: 1084: 1079: 1074: 1069: 1064: 1059: 1053: 1051: 1047: 1046: 1041: 1039: 1038: 1031: 1024: 1016: 1009: 1008: 1006: 1005: 1000: 994: 992: 983: 974: 971:Synoptic scale 963: 957: 956: 953: 952: 950: 949: 944: 939: 934: 929: 924: 918: 916: 912: 911: 909: 908: 903: 898: 893: 888: 883: 878: 872: 870: 863: 857: 856: 854: 853: 848: 843: 838: 833: 828: 823: 818: 813: 808: 803: 797: 795: 791: 790: 784:of the world ( 776: 774: 773: 766: 759: 751: 743: 742: 721:(2): 100–112. 701: 674: 648: 617: 576: 555:(4): 542–561. 535: 504: 478: 448: 425: 391: 355: 297: 256: 255: 253: 250: 234:weather models 187:in either the 172: 169: 146:Gulf of Mexico 138:Gulf of Panama 101: 98: 67:Gulf of Mexico 29:(precursor to 15: 13: 10: 9: 6: 4: 3: 2: 2435: 2424: 2421: 2419: 2416: 2414: 2411: 2410: 2408: 2393: 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1867: 1866: 1864: 1860: 1850: 1847: 1845: 1844:Icelandic Low 1842: 1840: 1837: 1836: 1834: 1830: 1819: 1815: 1812: 1808: 1807: 1805: 1801: 1794: 1790: 1787: 1783: 1780: 1776: 1773: 1769: 1766: 1762: 1759: 1755: 1752: 1748: 1745: 1741: 1738: 1734: 1731: 1727: 1724: 1720: 1717: 1713: 1710: 1706: 1703: 1699: 1696: 1692: 1689: 1685: 1682: 1678: 1675: 1671: 1668: 1664: 1661: 1657: 1654: 1650: 1647: 1643: 1640: 1636: 1633: 1629: 1626: 1622: 1619: 1615: 1612: 1608: 1605: 1601: 1598: 1594: 1591: 1587: 1584: 1580: 1577: 1573: 1570: 1566: 1563: 1559: 1556: 1552: 1549: 1545: 1542: 1538: 1537: 1535: 1531: 1524: 1520: 1517: 1513: 1510: 1506: 1503: 1499: 1496: 1492: 1489: 1485: 1482: 1478: 1475: 1471: 1468: 1464: 1461: 1457: 1454: 1450: 1447: 1443: 1440: 1436: 1433: 1429: 1426: 1422: 1419: 1415: 1412: 1408: 1405: 1401: 1398: 1394: 1391: 1387: 1386: 1384: 1380: 1373: 1369: 1366: 1362: 1359: 1355: 1352: 1348: 1345: 1341: 1340: 1338: 1334: 1329: 1318: 1314: 1311: 1307: 1304: 1300: 1297: 1293: 1292: 1290: 1286: 1281: 1273: 1268: 1266: 1261: 1259: 1254: 1253: 1250: 1246: 1243: 1239: 1229: 1226: 1224: 1221: 1219: 1216: 1214: 1211: 1209: 1206: 1205: 1203: 1199: 1188: 1187:November gale 1184: 1181: 1177: 1176: 1174: 1170: 1163: 1159: 1156: 1152: 1149: 1145: 1142: 1138: 1137: 1135: 1131: 1128: 1124: 1121: 1118:North America 1115: 1112: 1106: 1100: 1097: 1093: 1090: 1089: 1088: 1085: 1083: 1080: 1078: 1075: 1073: 1070: 1068: 1065: 1063: 1060: 1058: 1055: 1054: 1052: 1048: 1044: 1037: 1032: 1030: 1025: 1023: 1018: 1017: 1014: 1010: 1004: 1001: 999: 996: 995: 993: 991: 987: 984: 981:Surface-based 978: 975: 972: 967: 964: 962: 958: 948: 945: 943: 940: 938: 937:Kalahari High 935: 933: 930: 928: 925: 923: 920: 919: 917: 913: 907: 904: 902: 899: 897: 894: 892: 889: 887: 884: 882: 881:Siberian High 879: 877: 874: 873: 871: 867: 864: 862: 858: 852: 849: 847: 844: 842: 839: 837: 834: 832: 829: 827: 824: 822: 819: 817: 814: 812: 809: 807: 804: 802: 799: 798: 796: 792: 787: 783: 779: 772: 767: 765: 760: 758: 753: 752: 749: 737: 732: 728: 724: 720: 716: 712: 705: 702: 689: 685: 678: 675: 663: 659: 652: 649: 637: 632: 624: 622: 618: 612: 607: 603: 599: 595: 591: 587: 580: 577: 571: 566: 562: 558: 554: 550: 546: 539: 536: 524: 520: 513: 511: 509: 505: 493: 489: 482: 479: 466: 462: 455: 453: 449: 437:. AccuWeather 436: 429: 426: 414:. AccuWeather 413: 406: 404: 402: 400: 398: 396: 392: 379: 375: 368: 366: 364: 362: 360: 356: 350: 345: 341: 337: 333: 329: 325: 318: 316: 314: 312: 310: 308: 306: 304: 302: 298: 285: 281: 274: 272: 270: 268: 266: 264: 262: 258: 251: 249: 247: 243: 239: 235: 231: 226: 222: 218: 213: 209: 205: 200: 198: 194: 190: 186: 182: 181:tropical wave 178: 177:thunderstorms 170: 168: 166: 162: 158: 154: 149: 147: 143: 139: 135: 131: 127: 123: 119: 115: 106: 99: 97: 95: 91: 90:draw moisture 87: 83: 79: 75: 70: 68: 64: 60: 59:monsoonal low 56: 52: 51:Caribbean Sea 48: 44: 40: 32: 28: 23: 19: 2382: 2368: 2281:Funnel cloud 2199:Haida Eddies 2158:Polar vortex 1716:Herwart 2017 1709:Ophelia 2017 1632:St Jude 2013 1611:Joachim 2011 1590:Xynthia 2010 1548:Jeanett 2002 1533:21st century 1453:Charley 1986 1390:Ulysses 1903 1382:20th century 1336:19th century 1213:Hatteras low 1208:Aleutian Low 1148:Colorado low 1082:Weather bomb 782:anticyclones 718: 714: 704: 692:. Retrieved 687: 677: 665:. Retrieved 661: 651: 639:. Retrieved 635: 593: 589: 579: 552: 548: 538: 526:. Retrieved 522: 495:. Retrieved 491: 481: 469:. Retrieved 464: 439:. Retrieved 428: 416:. Retrieved 382:. Retrieved 377: 331: 327: 288:. Retrieved 283: 212:tropospheric 201: 174: 150: 134:Chivela Pass 111: 78:flash floods 71: 55:rainy season 42: 38: 36: 18: 2339:Steam devil 2259:Mesocyclone 2153:Cut-off low 2141:Upper level 1978:Subtropical 1948:Other areas 1893:Other areas 1869:Asiatic Low 1793:Ciarán 2023 1779:Larisa 2023 1772:Eunice 2022 1758:Aurore 2021 1751:Dennis 2020 1737:Adrian 2018 1702:Xavier 2017 1674:Niklas 2015 1625:Andrea 2012 1618:Dagmar 2011 1569:Kyrill 2007 1555:Gudrun 2005 1541:Oratia 2000 1523:Martin 1999 1516:Lothar 1999 1509:Anatol 1999 1411:Debbie 1961 1397:Iberia 1941 1162:Bighorn Low 1133:Lee Cyclone 1126:Continental 886:Azores High 861:Anticyclone 284:FOX Weather 157:anticyclone 2407:Categories 2344:Fire whirl 2334:Dust devil 2313:Waterspout 2274:Wall cloud 1986:Kona storm 1905:Kona storm 1786:Babet 2023 1765:Malik 2022 1744:Ciara 2020 1639:Xaver 2013 1597:Berit 2011 1583:Klaus 2009 1218:Nor'easter 841:Superstorm 378:Category 6 252:References 161:baroclinic 153:barotropic 2308:Landspout 2264:Supercell 2244:Whirlwind 2177:Mesoscale 1960:Sudestada 1927:Australia 1849:Genoa low 1695:Zeus 2017 1681:Egon 2017 1667:Tini 2014 1653:Anne 2014 1646:Dirk 2013 1576:Emma 2008 1488:Lili 1996 1087:Sting jet 846:Hypercane 694:4 January 667:4 January 641:4 January 528:4 January 497:4 January 471:4 January 465:LMTonline 441:4 January 418:4 January 384:4 January 290:4 January 244:tends to 130:vorticity 82:mudslides 2329:Gustnado 2222:Mesohigh 2217:Wake Low 2016:Tropical 1803:See also 1562:Per 2007 1223:Gulf low 1099:Rainband 1050:Concepts 794:Concepts 778:Cyclones 221:landfall 2286:Tornado 2062:Typhoon 2021:Outline 2006:Thermal 1201:Oceanic 1067:Cyclone 961:Cyclone 723:Bibcode 598:Bibcode 557:Bibcode 336:Bibcode 33:shown). 1900:Arctic 1241:Europe 690:. NASA 165:trough 140:, and 126:storms 2322:Minor 2252:Major 1832:Other 1172:Other 1062:Storm 990:Polar 806:Storm 223:as a 219:made 206:when 124:when 1862:Asia 1092:List 780:and 696:2024 669:2024 643:2024 530:2024 499:2024 473:2024 443:2024 420:2024 386:2024 292:2024 112:The 80:and 37:The 731:doi 606:doi 565:doi 492:CNN 344:doi 332:145 191:or 43:CAG 2409:: 729:. 719:12 717:. 713:. 686:. 660:. 634:. 620:^ 604:. 594:57 592:. 588:. 563:. 553:58 551:. 547:. 521:. 507:^ 490:. 463:. 451:^ 394:^ 376:. 358:^ 342:. 330:. 326:. 300:^ 282:. 260:^ 136:, 2023:) 2019:( 1271:e 1264:t 1257:v 1035:e 1028:t 1021:v 788:) 770:e 763:t 756:v 739:. 733:: 725:: 698:. 671:. 645:. 614:. 608:: 600:: 573:. 567:: 559:: 532:. 501:. 475:. 445:. 422:. 388:. 352:. 346:: 338:: 294:. 41:(

Index

Satellite image of a developing tropical disturbance
tropical cyclones
Hurricane Michael
area of low pressure
Caribbean Sea
rainy season
monsoonal low
counterclockwise circulation
Gulf of Mexico
Central America
flash floods
mudslides
Tropical cyclones
draw moisture
rainfall associated with tropical cyclones
Annotated satellite image of Central America and the surrounding waters
prevailing winds
blow from the east
Madden–Julian oscillation
storms
vorticity
Chivela Pass
Gulf of Panama
Gulf of Papagayo
Gulf of Mexico
barotropic
anticyclone
baroclinic
trough
thunderstorms

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