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Spatio-Temporal Variability of Rainfall Indices and their Teleconnections with El Nino-Southern Oscillation for Tapi Basin, India

机译:中国Tapi Basin的埃尔Nino-Southern振荡的降雨指数及其联信变异性的时空变化

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The long-term spatio-temporal variability in twelve rainfall indices across Tapi basin are investigated for period 1944-2013. The temporal trends in aforesaid indices, representing magnitude, intensity, frequency and duration of rainfall, are analysed using non-parametric tests. The total annual rainfall exhibit uniformly increasing trends over Lower Tapi basin (LTB), while heterogeneous trends are observed across Upper (UTB) and Middle (MTB) Tapi basins. The rainy days portrays decreasing trends at 75% stations in the basin, while rainfall intensity displays increasing trends across LTB and UTB. On other hand, LTB and Purna sub-catchment (in UTB) show coherent increasing trends in extreme rainfall, while decreasing trends are observed over Burhanpur sub-catchment (in UTB) and MTB. A considerable increase in duration of dry spells is reported at 92.5% stations in the basin, indicating a marked shift towards drier climatic regime. Further, Principal Component Analysis (PCA) is carried out to address the space-time variability of rainfall indices. The results of PCA were adopted in cluster analysis to identify the stations exhibiting similar characteristic variations in rainfall trends. The hydroclimatic teleconnections between rainfall indices and large-scale oceanic-atmospheric circulations of the tropical Pacific Ocean (viz., El Nino-Southern Oscillation) revealed the prevalence of wet conditions in the basin during moderate to strong La-Nina, while dry conditions were encountered during moderate to strong El-Nino and weak La-Nina events. The spatial estimates of rainfall indices are derived corresponding to 2-, 10- and 50-year return periods which would be helpful in hydrologic design and risk assessment of rainfall-induced disasters in near future.
机译:在Tapi盆地的十二个降雨指数中进行了长期时空变异,于1944 - 2013年期间进行了调查。使用非参数测试分析上述指标的时间趋势,代表降雨的幅度,强度,频率和持续时间。年降雨量总数呈均匀增加较低的小吃盆(LTB)趋势,而在上部(UTB)和中间(MTB)Tapi盆地上观察过异质趋势。雨天描绘了盆地中75%站的趋势下降,而降雨强度会显示LTB和UTB的增加趋势。在另一方面,LTB和Purna子集水区(在UTB)上显示出极端降雨的连贯趋势,同时在Burhanpur子集水区(UTB)和MTB上观察到趋势的降低。在盆地的92.5%站报告干法术持续时间相当大的增加,表明朝向干旱性气候制度的显着转变。此外,执行主成分分析(PCA)以解决降雨指数的时空变化。在集群分析中采用了PCA的结果,以确定呈现降雨趋势相似特征变异的站。热带太平洋降雨指数与大型海洋大气循环之间的循环互联网(埃尔Nino-Southern振荡)揭示了在中等至强La-Nina的盆地湿病症的患病率,而干燥条件是在中度到强大的el-nino和弱la-nino活动期间遇到。降雨指数的空间估计是对应于2-,10至50年和50年的回报期,这将有助于在不久的将来的水文设计和降雨造成灾害的风险评估。

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