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Horse latitudes

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3334: 3348: 252: 29: 316: 2290: 284:, which would favor the Japanese archipelago, while in La Niña years the formation of tropical cyclones, along with the subtropical ridge position, shift west, which increases the threat to China. In the Atlantic basin, the subtropical ridge position tends to lie about 5 degrees farther south during El Niño years, which leads to a more southerly recurvature for tropical cyclones during those years. 162:. This air mass rises and then diverges, moving away from the equator in both northerly and southerly directions. As the air moves towards the mid-latitudes on both sides of the equator, it cools and sinks. This creates a ridge of high pressure near the 30th parallel in both hemispheres. At the surface level, the sinking air diverges again with some returning to the equator, creating the 89:
called the "dead horse" time, and it usually lasted a month or two. The seaman's ceremony was to celebrate having worked off the "dead horse" debt. As west-bound shipping from Europe usually reached the subtropics at about the time the "dead horse" was worked off, the latitude became associated with the ceremony.
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A third explanation, which simultaneously explains both the northern and southern horse latitudes and does not depend on the length of the voyage or the port of departure, is based on maritime terminology: a ship was said to be 'horsed' when, although there was insufficient wind for sail, the vessel
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transported horses by ship to their colonies in the West Indies and Americas. Ships often became becalmed in mid-ocean in this latitude, thus severely prolonging the voyage; the resulting water shortages made it impossible for the crew to keep the horses alive, and they would throw the dead or dying
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The subtropical ridge starts migrating poleward in late spring reaching its zenith in early autumn before retreating equatorward during the late fall, winter, and early spring. The equatorward migration of the subtropical ridge during the cold season is due to increasing north-south temperature
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of a horse around the deck before throwing it overboard. Seamen were paid partly in advance before a long voyage, and they frequently spent their pay all at once, resulting in a period of time without income. If they got advances from the ship's paymaster, they would incur debt. This period was
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form on the side of the subtropical ridge closer to the equator, then move poleward past the ridge axis before recurving into the main belt of the Westerlies. When the subtropical ridge shifts due to ENSO, so will the preferred tropical cyclone tracks. Areas west of Japan and Korea tend to
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extend into the United States. The subtropical ridge across North America typically migrates far enough northward to begin monsoon conditions across the Desert Southwest from July to September. When the subtropical ridge is farther north than normal towards the
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In summer, On the subtropical ridge's western edge (generally on the eastern coast of continents), the high-pressure cell pushes poleward a southerly flow (northerly in the southern hemisphere) of tropical air. In the United States, the subtropical ridge
340:. When the high pressure moves south, its circulation cuts off the moisture, and the hot, dry continental airmass returns from the northwest, and therefore the atmosphere dries out across the Desert Southwest, causing a break in the monsoon regime. 119:, October 1967). He argued the maritime use of 'horsed' described a ship that was being carried along by an ocean current or tide in the manner of a rider on horseback. The term had been in use since the end of the seventeenth century. Furthermore, 668: 944: 981: 2845: 367:
When surface winds become light, the subsidence produced directly under the subtropical ridge can lead to a buildup of particulates in urban areas under the ridge, leading to widespread
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allowing for a more northerly axis for the ridge, while El Niños show flatter, more southerly ridges. The change of the ridge position during ENSO cycles changes the tracks of
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differences between the poles and tropics. The latitudinal movement of the subtropical ridge is strongly correlated with the progression of the monsoon trough or
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The consistently warm, dry, and sunny conditions of the horse latitudes are the main cause for the existence of the world's major hot deserts, such as the
739: 2800: 127:, an island off the coast of Brazil, mentions it had been visited frequently by ships "occasioned by the currents having horsed them to the westward". 177:
The subtropical ridge moves poleward during the summer, reaching its highest latitude in early autumn, before moving back during the cold season. The
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India Directory, or, Directions for Sailing to and from the East Indies, China, Australia, Cape of Good Hope, Brazil and the Interjacent Ports..
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that form around their equatorward and western peripheries. As the subtropical ridge varies in position and strength, it can enhance or depress
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India directory, or, Directions for sailing to and from the East Indies, China, Australia, Cape of Good Hope, Brazil, and the interjacent ports
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Interannual and Interdecadal Variations of the East Asian Summer Monsoon and Tropical Pacific SSTs. Part I: Roles of the Subtropical Ridge.
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The horse latitudes are associated with the subtropical anticyclone. The belt in the Northern Hemisphere is sometimes called the "calms of
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The subtropical ridge shows up as a large area of black (dryness) on this water vapor satellite image from September 2000.
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are German synonyms for a horse. An incorrect translation could therefore have produced the term "horse latitudes".
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A further explanation is that this naming first appeared in the English translation of a German book where
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A likely and documented explanation is that the term is derived from the "dead horse" ritual of seamen (see
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deserts in the southwestern United States and northern Mexico, all in the Northern Hemisphere; and the
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helps create the hot, sultry summers with daily thunderstorms with buoyant airmasses typical of the
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season for Asia. The subtropical ridge position is linked to how far northward monsoon moisture and
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When the subtropical ridge in the northwest Pacific is stronger than normal, it leads to a wet
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and neutral years, while mainland China experiences much greater landfall frequency during
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years. During El Niño years, the break in the subtropical ridge tends to lie near
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which during summer is reinforced by other climatological mechanisms such as the
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US Department of Commerce, National Oceanic and Atmospheric Administration.
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An alternative theory, of sufficient popularity to serve as an example of
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experience far fewer September–November tropical cyclone impacts during
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Bell, Gerald; Chelliah, Muthuvel; Mo, Kingste; Goldenberg, Stanley;
181:(ENSO) can displace the northern hemisphere subtropical ridge, with 3290: 3183: 3178: 2289: 2184: 2060: 398: 41: 774:
Journal of Climate: pp. 4310–4325. Retrieved on February 11, 2007.
170:. Many of the world's deserts are caused by these climatological 3247: 3023: 2028: 1922: 1739: 1481: 1065: 1026: 986: 337: 324: 310: 190: 53: 21:
This article is about the geographical area. For other uses, see
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A diagram showing the relative positions of the horse latitudes
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10.1175/1520-0442(2004)017<1419:IOENOE>2.0.CO;2
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Channel Video Productions. Retrieved on February 11, 2007.
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10.1175/1520-0442(2001)014<3192:SAASM>2.0.CO;2
474:, Sixth Edition. New York: Columbia University Press, 2003 376: 733: 84:). In this practice, the seaman paraded a straw-stuffed 785:
Basics of the Arizona Monsoon & Desert Meteorology.
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Latitudes 30–35 degrees north and south of the Equator
462:, London, Oxford University Press, 1976. pp. 233, 399 432: 805:
Review of Variability in the North American Monsoon.
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Wu, M. C.; Chang, W. L.; Leung, W. M. (March 2004).
200:" and that in the Southern Hemisphere the "calms of 109:
could make good progress by latching on to a strong
615: 336:, monsoon thunderstorms can spread northward into 770:C.-P. Chang, Yongsheng Zhang, and Tim Li (1999). 544:Rodwell, M. J.; Hoskins, B. J. (August 1, 2001). 3366: 871:University Corporation for Atmospheric Research 614:Roger Graham Barry, Richard J. Chorley (1992). 158:leads to large amounts of convection along the 2780:List of atmospheric pressure records in Europe 738:; Blake, Eric; Pasch, Richard (May 17, 2004). 546:"Subtropical Anticyclones and Summer Monsoons" 543: 2225: 1989: 1724: 945: 193:regimes around their low-latitude periphery. 692: 920:Physical Geography – The Global Environment 821:Environment: An Interdisciplinary Anthology 2232: 2218: 2003: 1996: 1982: 1731: 1717: 952: 938: 667:. United States Navy. 2006. Archived from 718: 589: 571: 561: 497: 460:The Oxford Companion to Ships and the Sea 299:Role in weather formation and air quality 3064:South-West Indian Ocean tropical cyclone 314: 250: 27: 2239: 925:Winds and the Global Circulation System 740:"NOAA: 2004 Atlantic Hurricane Outlook" 3367: 2213: 1977: 1712: 933: 375:rises towards 100 percent overnight, 75: 1950: 1813:Tropical cyclones and climate change 891:The Columbia Electronic Encyclopedia 472:The Columbia Electronic Encyclopedia 319:Mean July subtropical ridge position 3037:Mediterranean tropical-like cyclone 3030:North Indian Ocean tropical cyclone 2963:Mediterranean tropical-like cyclone 2846:East Asian-northwest Pacific storms 658:"3.3 JTWC Forecasting Philosophies" 13: 3125:Upper tropospheric cyclonic vortex 3071:Australian region tropical cyclone 880: 512:. London: W. H. Allen. p. 31. 14: 3411: 913: 873:. Retrieved on February 11, 2007. 810:. Retrieved on February 11, 2007. 783:Arizona State University (2009). 645:Atmosphere, weather, and climate. 289:Atlantic multidecadal oscillation 3346: 3332: 2288: 979: 618:Atmosphere, weather, and climate 219:deserts in the Middle East, the 154:The heating of the earth at the 23:Horse latitudes (disambiguation) 3085:South Atlantic tropical cyclone 3044:Black Sea tropical-like cyclone 853: 850:Retrieved on February 11, 2007. 833: 813: 808:United States Geological Survey 797: 794:Retrieved on February 11, 2007. 777: 764: 727: 686: 650: 435:"What are the Horse Latitudes?" 354:East Coast of the United States 3078:South Pacific tropical cyclone 2841:Continental North Asian storms 607: 598: 537: 516: 491: 477: 465: 452: 426: 404:Intertropical Convergence Zone 262:Intertropical Convergence Zone 160:Intertropical Convergence Zone 134:was incorrectly understood as 1: 419: 3400:Tropical cyclone meteorology 3339:Tropical cyclones portal 2380:Great Sheffield Gale of 1962 2320:Moray Firth fishing disaster 1863:Ridiculously Resilient Ridge 665:Joint Typhoon Warning Center 293:tropical cyclone development 246: 243:in the Southern Hemisphere. 179:El Niño–Southern Oscillation 149: 7: 3189:Mesoscale convective vortex 3171:Mesoscale convective system 2773:List of European windstorms 2190:Pacific Northwest windstorm 839:Myanmar government (2007). 382: 360:, southern Queensland and, 10: 3416: 846:February 24, 2008, at the 364:province in South Africa. 308: 302: 20: 3326: 3283: 3213: 3204: 3169: 3146: 3137: 3102: 3053: 2991: 2976: 2953:Australian east coast Low 2938: 2909: 2896:Australian east coast low 2888: 2879: 2854: 2823: 2793: 2764: 2494: 2436:1992 New Year's Day Storm 2343: 2297: 2286: 2249: 2209: 2202: 2162: 2133: 2094: 2087: 2078: 2069: 2011: 1973: 1941: 1930: 1921: 1876: 1830: 1821: 1755: 978: 975: 745:Climate Prediction Center 498:Horsburgh, James (1836). 168:Rodwell–Hoskins mechanism 100:originates from when the 60:ridges or highs. It is a 3385:Meteorological phenomena 2464:Boxing Day Storm of 1998 2457:Christmas Eve storm 1997 1793:Annular tropical cyclone 291:'s mode is favorable to 3253:Multiple-vortex tornado 2692:Friederike (David) 2018 2685:Eleanor (Burglind) 2018 2408:December 1981 windstorm 2366:North Sea flood of 1953 2279:Christmas Flood of 1717 905:Encyclopædia Britannica 899:"Horse Latitudes"  803:David K. Adams (2009). 524:Hadley Circulation Cell 389:Atmospheric circulation 3194:Line echo wave pattern 3148:Mesoscale ocean eddies 2917:Southern Ocean cyclone 2005:Extratropical cyclones 1798:Bar (tropical cyclone) 1788:Central dense overcast 908:(11th ed.). 1911. 859:Robert Tardif (2002). 530:March 5, 2009, at the 320: 256: 64:at the divergence of 33: 2566:Friedhelm/Bawbag 2011 2429:Burns' Day storm 1990 2313:Night of the Big Wind 2034:Post-tropical cyclone 1783:Rapid intensification 887:Horse latitudes entry 866:May 20, 2011, at the 790:May 31, 2009, at the 622:. Routledge. p.  500:"Fernando de Noronha" 439:oceanservice.noaa.gov 318: 254: 31: 3353:Tornadoes portal 3263:Anticyclonic tornado 3231:Low-topped supercell 3009:Cape Verde hurricane 2401:Gale of January 1976 861:Fog characteristics. 736:Landsea, Christopher 371:. If the low-level 116:Journal of Geography 82:Beating a dead horse 3375:Circles of latitude 3055:Southern Hemisphere 2993:Northern Hemisphere 2881:Southern Hemisphere 2836:Western Disturbance 2650:Thomas (Doris) 2017 2422:Great storm of 1987 2387:1968 Scotland storm 2327:Tay Bridge disaster 2306:Great Storm of 1824 2272:Great Storm of 1703 2242:European windstorms 2071:Northern Hemisphere 1889:South Atlantic High 1877:Southern Hemisphere 1853:North American High 1831:Northern Hemisphere 1076:Tropic of Capricorn 1037:Tropic of Capricorn 998:Tropic of Capricorn 961:Circles of latitude 711:2004JCli...17.1419W 563:2001JCli...14.3192R 522:Owen E. Thompson. " 172:high-pressure areas 125:Fernando de Noronha 121:The India Directory 105:animals overboard. 96:, is that the term 3002:Atlantic hurricane 2958:Lake Huron cyclone 2019:Anticyclonic storm 1894:South Pacific High 1858:North Pacific High 1773:High-pressure area 1763:Anticyclonic storm 752:on January 1, 2019 699:Journal of Climate 550:Journal of Climate 485:"World Wide Words" 394:Circle of latitude 321: 257: 76:Origin of the term 62:high-pressure area 34: 3362: 3361: 3322: 3321: 3318: 3317: 3314: 3313: 3258:Satellite tornado 3133: 3132: 3098: 3097: 3094: 3093: 3018:Pacific hurricane 2934: 2933: 2930: 2929: 2875: 2874: 2819: 2818: 2789: 2788: 2334:Eyemouth disaster 2250:14th-18th century 2198: 2197: 2158: 2157: 2039:Low-pressure area 1917: 1916: 1909:Subtropical ridge 1868:Subtropical ridge 1778:Low-pressure area 1748:Centers of action 1706: 1705: 633:978-0-415-07760-6 556:(15): 3192–3211. 373:relative humidity 269:tropical cyclones 241:Australian Desert 187:tropical cyclones 123:in its entry for 44:about 30 degrees 3407: 3351: 3350: 3349: 3337: 3336: 3335: 3211: 3210: 3144: 3143: 3087: 3080: 3073: 3066: 3056: 3046: 3039: 3032: 3020: 3011: 3004: 2994: 2989: 2988: 2901:Black nor'easter 2886: 2885: 2882: 2801:Black Sea storms 2782: 2775: 2757: 2750: 2743: 2736: 2729: 2722: 2715: 2708: 2701: 2694: 2687: 2680: 2673: 2666: 2659: 2652: 2645: 2638: 2631: 2624: 2617: 2610: 2603: 2596: 2589: 2582: 2575: 2568: 2561: 2554: 2547: 2540: 2533: 2526: 2519: 2512: 2505: 2487: 2480: 2473: 2466: 2459: 2452: 2445: 2443:Braer Storm 1993 2438: 2431: 2424: 2417: 2410: 2403: 2396: 2389: 2382: 2375: 2368: 2361: 2354: 2336: 2329: 2322: 2315: 2308: 2292: 2281: 2274: 2267: 2260: 2244: 2234: 2227: 2220: 2211: 2210: 2207: 2206: 2151: 2144: 2126: 2119: 2112: 2105: 2092: 2091: 2085: 2084: 2081: 2076: 2075: 2072: 1998: 1991: 1984: 1975: 1974: 1948: 1947: 1944: 1939: 1938: 1935: 1928: 1927: 1884:South Polar High 1838:North Polar High 1828: 1827: 1733: 1726: 1719: 1710: 1709: 1086:Antarctic Circle 1071:Tropic of Cancer 1047:Antarctic Circle 1032:Tropic of Cancer 1008:Antarctic Circle 993:Tropic of Cancer 983: 954: 947: 940: 931: 930: 909: 901: 874: 857: 851: 837: 831: 817: 811: 801: 795: 781: 775: 768: 762: 761: 759: 757: 748:. Archived from 731: 725: 724: 722: 705:(6): 1419–1428. 690: 684: 683: 681: 679: 673: 662: 654: 648: 647: 642: 640: 621: 611: 605: 602: 596: 595: 593: 575: 565: 541: 535: 520: 514: 513: 495: 489: 488: 481: 475: 469: 463: 456: 450: 449: 447: 445: 430: 3415: 3414: 3410: 3409: 3408: 3406: 3405: 3404: 3365: 3364: 3363: 3358: 3347: 3345: 3333: 3331: 3310: 3279: 3200: 3165: 3129: 3090: 3083: 3076: 3069: 3062: 3054: 3049: 3042: 3035: 3028: 3016: 3007: 3000: 2992: 2980: 2972: 2926: 2905: 2880: 2871: 2850: 2815: 2785: 2778: 2771: 2760: 2753: 2746: 2739: 2732: 2725: 2718: 2711: 2704: 2697: 2690: 2683: 2676: 2669: 2662: 2655: 2648: 2641: 2634: 2627: 2620: 2613: 2606: 2599: 2592: 2585: 2578: 2571: 2564: 2557: 2550: 2543: 2536: 2529: 2522: 2515: 2508: 2501: 2490: 2483: 2476: 2469: 2462: 2455: 2448: 2441: 2434: 2427: 2420: 2413: 2406: 2399: 2392: 2385: 2378: 2371: 2364: 2357: 2350: 2339: 2332: 2325: 2318: 2311: 2304: 2293: 2284: 2277: 2270: 2265:Burchardi flood 2263: 2258:Grote Mandrenke 2256: 2245: 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1092:Horse latitudes 1088: 1083: 1078: 1073: 1068: 1063: 1060:Horse latitudes 1056: 1053:Horse latitudes 1049: 1044: 1039: 1034: 1029: 1024: 1021:Horse latitudes 1017: 1014:Horse latitudes 1010: 1005: 1000: 995: 990: 971: 969:Horse latitudes 958: 916: 896: 883: 881:Further reading 878: 877: 868:Wayback Machine 858: 854: 848:Wayback Machine 838: 834: 819:Adelson, Glen; 818: 814: 802: 798: 792:Wayback Machine 782: 778: 769: 765: 755: 753: 732: 728: 691: 687: 677: 675: 674:on July 5, 2012 671: 660: 656: 655: 651: 638: 636: 634: 612: 608: 603: 599: 542: 538: 532:Wayback Machine 521: 517: 496: 492: 483: 482: 478: 470: 466: 457: 453: 443: 441: 431: 427: 422: 414:Roaring Forties 385: 313: 307: 301: 249: 237:Kalahari Desert 211:in Africa, the 156:thermal equator 152: 98:horse latitudes 78: 38:horse latitudes 26: 19: 12: 11: 5: 3413: 3403: 3402: 3397: 3392: 3387: 3382: 3377: 3360: 3359: 3357: 3356: 3342: 3327: 3324: 3323: 3320: 3319: 3316: 3315: 3312: 3311: 3309: 3308: 3303: 3298: 3293: 3287: 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2622:Christina 2014 2618: 2611: 2604: 2597: 2590: 2583: 2576: 2569: 2562: 2555: 2548: 2541: 2534: 2527: 2520: 2513: 2506: 2498: 2496: 2492: 2491: 2489: 2488: 2481: 2474: 2467: 2460: 2453: 2446: 2439: 2432: 2425: 2418: 2411: 2404: 2397: 2394:Quimburga 1972 2390: 2383: 2376: 2369: 2362: 2355: 2347: 2345: 2341: 2340: 2338: 2337: 2330: 2323: 2316: 2309: 2301: 2299: 2295: 2294: 2287: 2285: 2283: 2282: 2275: 2268: 2261: 2253: 2251: 2247: 2246: 2237: 2236: 2229: 2222: 2214: 2204: 2200: 2199: 2196: 2195: 2193: 2192: 2187: 2182: 2177: 2172: 2166: 2164: 2160: 2159: 2156: 2155: 2153: 2152: 2145: 2142:Panhandle hook 2137: 2135: 2131: 2130: 2128: 2127: 2120: 2113: 2106: 2098: 2096: 2089: 2082: 2073: 2067: 2066: 2064: 2063: 2058: 2057: 2056: 2046: 2041: 2036: 2031: 2026: 2021: 2015: 2013: 2009: 2008: 2001: 2000: 1993: 1986: 1978: 1971: 1970: 1968: 1967: 1962: 1956: 1954: 1945: 1936: 1933:Synoptic scale 1925: 1919: 1918: 1915: 1914: 1912: 1911: 1906: 1901: 1896: 1891: 1886: 1880: 1878: 1874: 1873: 1871: 1870: 1865: 1860: 1855: 1850: 1845: 1840: 1834: 1832: 1825: 1819: 1818: 1816: 1815: 1810: 1805: 1800: 1795: 1790: 1785: 1780: 1775: 1770: 1765: 1759: 1757: 1753: 1752: 1746:of the world ( 1736: 1735: 1728: 1721: 1713: 1704: 1703: 1695: 1690: 1685: 1680: 1675: 1670: 1665: 1660: 1653: 1648: 1643: 1638: 1628: 1623: 1618: 1613: 1608: 1601: 1596: 1591: 1586: 1576: 1571: 1566: 1561: 1556: 1551: 1546: 1541: 1536: 1531: 1526: 1521: 1516: 1511: 1506: 1501: 1496: 1491: 1486: 1479: 1474: 1469: 1464: 1459: 1454: 1449: 1444: 1439: 1434: 1429: 1424: 1419: 1414: 1409: 1404: 1399: 1394: 1389: 1384: 1379: 1374: 1369: 1364: 1359: 1354: 1349: 1344: 1339: 1334: 1329: 1324: 1319: 1314: 1309: 1304: 1299: 1294: 1289: 1284: 1279: 1274: 1269: 1264: 1259: 1254: 1249: 1244: 1239: 1234: 1229: 1224: 1219: 1214: 1209: 1204: 1199: 1194: 1189: 1184: 1179: 1174: 1169: 1164: 1159: 1154: 1149: 1144: 1139: 1134: 1129: 1124: 1119: 1106: 1096: 1089: 1084: 1079: 1074: 1069: 1064: 1057: 1050: 1045: 1040: 1035: 1030: 1025: 1018: 1011: 1006: 1001: 996: 991: 984: 977: 976: 973: 972: 957: 956: 949: 942: 934: 928: 927: 922: 915: 914:External links 912: 911: 910: 894: 882: 879: 876: 875: 852: 832: 823:, pp. 466–467 812: 796: 776: 763: 726: 685: 649: 632: 606: 597: 536: 515: 490: 476: 464: 451: 424: 423: 421: 418: 417: 416: 411: 406: 401: 396: 391: 384: 381: 350:Gulf of Mexico 309:Main article: 300: 297: 248: 245: 229:Atacama Desert 151: 148: 94:folk etymology 77: 74: 17: 9: 6: 4: 3: 2: 3412: 3401: 3398: 3396: 3393: 3391: 3390:Climate zones 3388: 3386: 3383: 3381: 3378: 3376: 3373: 3372: 3370: 3355: 3354: 3343: 3341: 3340: 3329: 3328: 3325: 3307: 3304: 3302: 3299: 3297: 3294: 3292: 3289: 3288: 3286: 3282: 3276: 3273: 3271: 3268: 3264: 3261: 3259: 3256: 3254: 3251: 3250: 3249: 3246: 3244: 3241: 3237: 3234: 3232: 3229: 3227: 3224: 3223: 3222: 3219: 3218: 3216: 3212: 3209: 3207: 3203: 3195: 3192: 3191: 3190: 3187: 3185: 3182: 3180: 3177: 3176: 3174: 3172: 3168: 3162: 3159: 3157: 3156:Catalina eddy 3154: 3153: 3151: 3149: 3145: 3142: 3140: 3136: 3126: 3123: 3121: 3118: 3116: 3113: 3111: 3110:Cold-core low 3108: 3107: 3105: 3101: 3086: 3082: 3079: 3075: 3072: 3068: 3065: 3061: 3060: 3058: 3052: 3045: 3041: 3038: 3034: 3031: 3027: 3025: 3022: 3019: 3015: 3010: 3006: 3005: 3003: 2999: 2998: 2996: 2990: 2987: 2984: 2979: 2975: 2969: 2966: 2964: 2961: 2959: 2956: 2954: 2951: 2949: 2946: 2945: 2943: 2941: 2937: 2923: 2920: 2918: 2915: 2914: 2912: 2908: 2902: 2899: 2897: 2894: 2893: 2891: 2887: 2884: 2878: 2868: 2865: 2863: 2860: 2859: 2857: 2853: 2847: 2844: 2842: 2839: 2837: 2834: 2832: 2829: 2828: 2826: 2822: 2812: 2809: 2807: 2806:Icelandic Low 2804: 2802: 2799: 2798: 2796: 2792: 2781: 2777: 2774: 2770: 2769: 2767: 2763: 2756: 2752: 2749: 2745: 2742: 2738: 2735: 2731: 2728: 2724: 2721: 2717: 2714: 2710: 2707: 2703: 2700: 2696: 2693: 2689: 2686: 2682: 2679: 2675: 2672: 2668: 2665: 2661: 2658: 2654: 2651: 2647: 2644: 2640: 2637: 2633: 2630: 2626: 2623: 2619: 2616: 2612: 2609: 2605: 2602: 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2035: 2032: 2030: 2027: 2025: 2022: 2020: 2017: 2016: 2014: 2010: 2006: 1999: 1994: 1992: 1987: 1985: 1980: 1979: 1976: 1972: 1966: 1963: 1961: 1958: 1957: 1955: 1953: 1949: 1946: 1943:Surface-based 1940: 1937: 1934: 1929: 1926: 1924: 1920: 1910: 1907: 1905: 1902: 1900: 1899:Kalahari High 1897: 1895: 1892: 1890: 1887: 1885: 1882: 1881: 1879: 1875: 1869: 1866: 1864: 1861: 1859: 1856: 1854: 1851: 1849: 1846: 1844: 1843:Siberian High 1841: 1839: 1836: 1835: 1833: 1829: 1826: 1824: 1820: 1814: 1811: 1809: 1806: 1804: 1801: 1799: 1796: 1794: 1791: 1789: 1786: 1784: 1781: 1779: 1776: 1774: 1771: 1769: 1766: 1764: 1761: 1760: 1758: 1754: 1749: 1745: 1741: 1734: 1729: 1727: 1722: 1720: 1715: 1714: 1711: 1698: 1693: 1688: 1683: 1678: 1673: 1668: 1663: 1658: 1657: 1651: 1646: 1641: 1636: 1635: 1631: 1626: 1621: 1616: 1611: 1606: 1605: 1599: 1594: 1589: 1584: 1583: 1579: 1574: 1569: 1564: 1559: 1554: 1549: 1544: 1539: 1534: 1529: 1524: 1519: 1514: 1509: 1504: 1499: 1494: 1489: 1484: 1483: 1477: 1472: 1467: 1462: 1457: 1452: 1447: 1442: 1437: 1432: 1427: 1422: 1417: 1412: 1407: 1402: 1397: 1392: 1387: 1382: 1377: 1372: 1367: 1362: 1357: 1352: 1347: 1342: 1337: 1332: 1327: 1322: 1317: 1312: 1307: 1302: 1297: 1292: 1287: 1282: 1277: 1272: 1267: 1262: 1257: 1252: 1247: 1242: 1237: 1232: 1227: 1222: 1217: 1212: 1207: 1202: 1197: 1192: 1187: 1182: 1177: 1172: 1167: 1162: 1157: 1152: 1147: 1142: 1137: 1132: 1127: 1122: 1117: 1116: 1113: 1110: 1105: 1101: 1100: 1094: 1093: 1087: 1082: 1081:Arctic Circle 1077: 1072: 1067: 1062: 1061: 1055: 1054: 1048: 1043: 1042:Arctic Circle 1038: 1033: 1028: 1023: 1022: 1016: 1015: 1009: 1004: 1003:Arctic Circle 999: 994: 989: 988: 982: 974: 970: 966: 962: 955: 950: 948: 943: 941: 936: 935: 932: 926: 923: 921: 918: 917: 907: 906: 900: 895: 892: 888: 885: 884: 872: 869: 865: 862: 856: 849: 845: 842: 836: 830: 826: 822: 816: 809: 806: 800: 793: 789: 786: 780: 773: 767: 751: 747: 746: 741: 737: 730: 721: 716: 712: 708: 704: 700: 696: 689: 670: 666: 659: 653: 646: 635: 629: 625: 620: 619: 610: 601: 592: 587: 583: 579: 574: 569: 564: 559: 555: 551: 547: 540: 533: 529: 525: 519: 511: 507: 506: 501: 494: 486: 480: 473: 468: 461: 458:Kemp, Peter. 455: 440: 436: 429: 425: 415: 412: 410: 407: 405: 402: 400: 397: 395: 392: 390: 387: 386: 380: 378: 374: 370: 365: 363: 362:KwaZulu-Natal 359: 355: 351: 347: 341: 339: 335: 330: 329:thunderstorms 326: 317: 312: 306: 305:Air pollution 296: 294: 290: 285: 283: 279: 275: 270: 265: 263: 253: 244: 242: 238: 234: 230: 226: 222: 218: 214: 210: 209:Sahara Desert 205: 203: 199: 194: 192: 188: 184: 180: 175: 173: 169: 165: 161: 157: 147: 145: 141: 137: 133: 128: 126: 122: 118: 117: 112: 106: 103: 99: 95: 90: 87: 83: 73: 71: 67: 63: 59: 55: 51: 47: 43: 39: 30: 24: 16: 3395:Anticyclones 3344: 3330: 3243:Funnel cloud 3161:Haida Eddies 3120:Polar vortex 2678:Herwart 2017 2671:Ophelia 2017 2594:St Jude 2013 2573:Joachim 2011 2552:Xynthia 2010 2510:Jeanett 2002 2495:21st century 2415:Charley 1986 2352:Ulysses 1903 2344:20th century 2298:19th century 2175:Hatteras low 2170:Aleutian Low 2110:Colorado low 2044:Weather bomb 1744:anticyclones 1655: 1632: 1603: 1580: 1480: 1107: 1103: 1098: 1097: 1091: 1090: 1059: 1058: 1052: 1051: 1020: 1019: 1013: 1012: 985: 968: 967:showing the 903: 890: 855: 835: 820: 815: 799: 779: 766: 756:February 11, 754:. Retrieved 750:the original 743: 729: 702: 698: 688: 678:February 11, 676:. Retrieved 669:the original 664: 652: 644: 637:. Retrieved 617: 609: 600: 553: 549: 539: 518: 509: 504: 493: 479: 471: 467: 459: 454: 442:. Retrieved 438: 428: 366: 346:Bermuda High 342: 334:Four Corners 322: 286: 266: 258: 233:Namib Desert 206: 195: 176: 153: 143: 139: 136:Pferdbreiten 135: 131: 129: 120: 114: 107: 97: 91: 79: 37: 35: 15: 3380:Age of Sail 3301:Steam devil 3221:Mesocyclone 3115:Cut-off low 3103:Upper level 2940:Subtropical 2910:Other areas 2855:Other areas 2831:Asiatic Low 2755:Ciarán 2023 2741:Larisa 2023 2734:Eunice 2022 2720:Aurore 2021 2713:Dennis 2020 2699:Adrian 2018 2664:Xavier 2017 2636:Niklas 2015 2587:Andrea 2012 2580:Dagmar 2011 2531:Kyrill 2007 2517:Gudrun 2005 2503:Oratia 2000 2485:Martin 1999 2478:Lothar 1999 2471:Anatol 1999 2373:Debbie 1961 2359:Iberia 1941 2124:Bighorn Low 2095:Lee Cyclone 2088:Continental 1848:Azores High 1823:Anticyclone 639:November 9, 409:Polar front 164:Hadley cell 132:Rossbreiten 66:trade winds 58:subtropical 3369:Categories 3306:Fire whirl 3296:Dust devil 3275:Waterspout 3236:Wall cloud 2948:Kona storm 2867:Kona storm 2748:Babet 2023 2727:Malik 2022 2706:Ciara 2020 2601:Xaver 2013 2559:Berit 2011 2545:Klaus 2009 2180:Nor'easter 1803:Superstorm 829:0300110774 420:References 379:can form. 303:See also: 239:, and the 70:westerlies 3270:Landspout 3226:Supercell 3206:Whirlwind 3139:Mesoscale 2922:Sudestada 2889:Australia 2811:Genoa low 2657:Zeus 2017 2643:Egon 2017 2629:Tini 2014 2615:Anne 2014 2608:Dirk 2013 2538:Emma 2008 2450:Lili 1996 2049:Sting jet 1808:Hypercane 965:Meridians 582:0894-8755 444:April 17, 287:When the 247:Migration 202:Capricorn 150:Formation 42:latitudes 40:are the 3291:Gustnado 3184:Mesohigh 3179:Wake Low 2978:Tropical 2765:See also 2524:Per 2007 2185:Gulf low 2061:Rainband 2012:Concepts 1756:Concepts 1740:Cyclones 864:Archived 844:Archived 788:Archived 591:58891085 528:Archived 399:Doldrums 383:See also 352:and the 68:and the 3248:Tornado 3024:Typhoon 2983:Outline 2968:Thermal 2163:Oceanic 2029:Cyclone 1923:Cyclone 1066:Equator 1027:Equator 987:Equator 707:Bibcode 558:Bibcode 487:. 2008. 338:Arizona 325:monsoon 311:Monsoon 278:La Niña 274:El Niño 225:Sonoran 213:Arabian 191:monsoon 183:La Niña 111:current 102:Spanish 54:Equator 52:of the 2862:Arctic 2203:Europe 827:  630:  588:  580:  358:Pampas 235:, the 231:, the 221:Mojave 217:Syrian 198:Cancer 86:effigy 3284:Minor 3214:Major 2794:Other 2134:Other 2024:Storm 1952:Polar 1768:Storm 1697:45x90 1692:45x90 1687:45x90 1682:45x90 841:Haze. 672:(PDF) 661:(PDF) 586:S2CID 282:130°E 267:Most 140:Pferd 50:south 46:north 2824:Asia 2054:List 1742:and 1476:170° 1471:160° 1466:140° 1461:130° 1456:110° 1451:100° 1416:170° 1411:160° 1406:140° 1401:130° 1396:110° 1391:100° 1356:175° 1351:165° 1346:155° 1341:145° 1336:135° 1331:125° 1326:115° 1321:105° 1266:175° 1261:165° 1256:155° 1251:145° 1246:135° 1241:125° 1236:115° 1231:105° 1176:180° 1171:150° 1166:120° 1146:180° 1141:150° 1136:120° 825:ISBN 758:2007 680:2007 641:2009 628:ISBN 578:ISSN 446:2021 369:haze 223:and 215:and 144:Ross 142:and 48:and 36:The 1677:85° 1672:75° 1667:65° 1662:55° 1656:45° 1650:35° 1645:25° 1640:15° 1625:85° 1620:75° 1615:65° 1610:55° 1604:45° 1598:35° 1593:25° 1588:15° 1573:90° 1568:80° 1563:70° 1558:60° 1553:50° 1548:40° 1543:30° 1538:20° 1533:10° 1528:90° 1523:80° 1518:70° 1513:60° 1508:50° 1503:40° 1498:30° 1493:20° 1488:10° 1446:80° 1441:70° 1436:50° 1431:40° 1426:20° 1421:10° 1386:80° 1381:70° 1376:50° 1371:40° 1366:20° 1361:10° 1316:95° 1311:85° 1306:75° 1301:65° 1296:55° 1291:45° 1286:35° 1281:25° 1276:15° 1226:95° 1221:85° 1216:75° 1211:65° 1206:55° 1201:45° 1196:35° 1191:25° 1186:15° 1161:90° 1156:60° 1151:30° 1131:90° 1126:60° 1121:30° 889:in 715:doi 624:117 568:doi 526:". 377:fog 204:". 3371:: 1630:5° 1578:5° 1482:0° 1271:5° 1181:5° 1112:0° 963:/ 902:. 742:. 713:. 703:17 701:. 697:. 663:. 643:. 626:. 584:. 576:. 566:. 554:14 552:. 548:. 508:. 502:. 437:. 264:. 174:. 72:. 2985:) 2981:( 2233:e 2226:t 2219:v 1997:e 1990:t 1983:v 1750:) 1732:e 1725:t 1718:v 1634:S 1582:N 1115:E 1109:W 953:e 946:t 939:v 760:. 723:. 717:: 709:: 682:. 594:. 570:: 560:: 534:. 448:. 25:.

Index

Horse latitudes (disambiguation)

latitudes
north
south
Equator
subtropical
high-pressure area
trade winds
westerlies
Beating a dead horse
effigy
folk etymology
Spanish
current
Journal of Geography
Fernando de Noronha
thermal equator
Intertropical Convergence Zone
Hadley cell
Rodwell–Hoskins mechanism
high-pressure areas
El Niño–Southern Oscillation
La Niña
tropical cyclones
monsoon
Cancer
Capricorn
Sahara Desert
Arabian

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