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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Heat and moisture budgets of the Walker circulation and associated rainfall anomalies during El Nino events
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Heat and moisture budgets of the Walker circulation and associated rainfall anomalies during El Nino events

机译:厄尔尼诺事件期间沃克环流的热量和水分预算以及相关的降水异常

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Large-scale aspects of the heat and moisture budgets of the Walker circulation (WC) are analysed for the austral summer during the period from 1970 to 2000. Since several earlier studies discuss theoretical and modelling aspects of the heat and moisture budgets of the WC, our main objective is to make an observational analysis of such budgets, including a composite of five strong El Nino-southern oscillation events covered by the period of study. For this purpose, data from the National Centers for Environmental Prediction-National Center for Atmospheric Research reanalysis and Global Precipitation Climatology Project are used. Analysis of the moisture budget in the near-equatorial regions of the Southern Hemisphere showed that the three continents (South America, Africa and maritime continents) are characterized by high precipitation and that low precipitation occurs in the intermediate oceans. Regions of high (low) precipitation are associated with the vertically integrated moisture flux convergence (divergence). Analysis of the heat budget for the WC showed, as deduced in some theoretical studies, that the diabatic heating (cooling) is balanced by adiabatic cooling (heating) over regions with a convective (non-convective) regime. The loss of radiation to space over non-convective areas is balanced by adiabatic heating due to the sinking motion. There is heating over the continents, probably associated with the ascending motion in the WC, and cooling over the intermediate oceans, which is related to the loss of radiation in the descending branch of the WC. Analysis of the moisture balance for the entire period and a composite of El Ni?o periods shows that the WC is associated with precipitation variations in the near-equatorial regions of the continents. The low-level changes in the WC are associated with the moisture flux changes and have the main role in the maintenance of the rainfall anomalies during the El Nino events.
机译:对沃克环流(WC)1970年至2000年夏季南方的热量和水分预算的大规模方面进行了分析。由于较早的研究讨论了WC热量和水分预算的理论和模型方面,我们的主要目标是对此类预算进行观察性分析,包括研究期间涵盖的五个强烈的厄尔尼诺-南方振荡事件的综合。为此,使用了来自国家环境预测中心-国家大气研究再分析中心和全球降水气候学项目的数据。对南半球近赤道区域的水分收支进行的分析表明,这三个大陆(南美,非洲和海洋大陆)的特征是高降水量,而中层海洋则出现低降水量。高(低)降水量区域与垂直积分的水分通量会聚(发散)有关。根据一些理论研究得出的结论,WC的热量收支分析表明,在对流(非对流)状态下,绝热加热(冷却)与绝热冷却(加热)是平衡的。由于下沉运动,通过绝热加热来平衡辐射到非对流区域上方的空间的损失。大陆上的加热可能与WC的上升运动有关,而中间海洋的冷却则与WC下降分支中的辐射损失有关。对整个时期和El Ni?o时期综合的水分平衡的分析表明,WC与该大陆近赤道区域的降水变化有关。 WC的低水平变化与水分通量变化有关,并且在维护El Nino事件期间的降雨异常中起主要作用。

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