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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >The coincidence of daily rainfall events in Liberia, Costa Rica and tropical cyclones in the Caribbean basin
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The coincidence of daily rainfall events in Liberia, Costa Rica and tropical cyclones in the Caribbean basin

机译:利比里亚,哥斯达黎加和加勒比海盆地热带气旋的每日降雨事件同时发生

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The occurrence of tropical cyclones in the Caribbean and North Atlantic basins has been previously noted to have a significant effect both upon individual hydro-climatological events as well as on the quantity of annual precipitation experienced along the Pacific flank of Central America. A methodology for examining the so-called 'indirect effects' of tropical cyclones (i.e. those effects resulting front a tropical cyclone at a considerable distance from the area of interest) on a daily rainfall record is established, which uses a variant of contingency table analysis. The method is tested using a single station on the Pacific slope of Costa Rica. Employing daily precipitation records from Liberia, north-western Costa Rica (1964-1995), and historic storm tracks of tropical cyclones in the North Atlantic, it is determined that precipitation falling in coincidence with the passage of tropical depressions, tropical storms, and hurricanes accounts for approximately 15% of average annual precipitation. The greatest effects are associated with storms passing within 1300 km of the precipitation station, and are most apparent in the increased frequency of daily rainfall totals in the range of 40-60 mm, rather than in the largest daily totals. The complexity and nonstationarity of factors affecting precipitation in this region are reflected in the decline in the number of tropical cyclones and their significance to annual precipitation totals after 1980, simultaneous to an increase in annual precipitation totals. The methodology employed in this study is shown to be a useful toot in illuminating the indirect effects of tropical cyclones in the region, with the potential for application in other areas. Copyright (c) 2005 Royal Meteorological Society.
机译:以前已经注意到,加勒比和北大西洋盆地的热带气旋的发生对单个的水文气候事件以及中美洲太平洋沿岸的年降水量都具有重大影响。建立了一种方法,用于检查日降水记录上所谓的热带气旋的“间接影响”(即,导致热带气旋在距目标区域相当远的距离前产生的那些影响)的方法,该方法使用了列联表分析方法。使用哥斯达黎加太平洋斜坡上的一个站点测试该方法。利用利比里亚,哥斯达黎加西北部(1964-1995)的每日降水记录以及北大西洋的热带气旋的历史风暴轨迹,可以确定降水量与热带低气压,热带风暴和飓风的通过同时下降约占年平均降水量的15%。最大的影响与在降水站1300 km内经过的暴风雨有关,并且最明显的是日降水总量增加的频率在40-60 mm范围内,而不是最大的日总量。影响该地区降水的因素的复杂性和非平稳性反映在热带气旋数量的减少及其对1980年以后年降水总量的影响上,同时年降水总量也有所增加。这项研究中使用的方法论被证明是阐明该地区热带气旋间接影响的有用工具,并有可能在其他地区应用。版权所有(c)2005皇家气象学会。

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