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首页> 外文期刊>Climate research >Influence of El Nino/southern oscillation, Pacific decadal oscillation, and local sea-surface temperature anomalies on peak season monsoon precipitation in India
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Influence of El Nino/southern oscillation, Pacific decadal oscillation, and local sea-surface temperature anomalies on peak season monsoon precipitation in India

机译:El Nino /南部振荡,太平洋年代际振荡和局部海表温度异常对印度季风季风降水的影响

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摘要

Many modeling and empirical studies have revealed that summer monsoon precipitation in India is significantly affected by El Nino/Southern Oscillation (ENSO) as well as by sea-surface temperatures (SSTs) in the Arabian Sea, Bay of Bengal, and Indian Ocean. Recently, the impact of the Pacific decadal oscillation (PDO) on Indian rainfall has been the focus of research. In this investigation, we collect monthly rainfall data for 18 grid cells covering India and develop statistical indices of ENSO, PDO, and local SSTs over the period 1925-1998. We find that ENSO reduces precipitation in southern India while having a small impact over most of the country. The PDO appears to amplify the ENSO signal in southern India, while local SSTs were directly related to monsoon precipitation totals in the southern peninsula region. While the associations are often statistically significant, the combination of ENSO, PDO, and SSTs explains less than 20% of the variance in monsoon rainfall throughout India. [References: 39]
机译:许多模型和经验研究表明,印度的夏季季风降水受厄尔尼诺/南方涛动(ENSO)以及阿拉伯海,孟加拉湾和印度洋的海表温度(SST)的影响很大。最近,太平洋年代际振荡(PDO)对印度降水的影响已成为研究重点。在这项调查中,我们收集了覆盖印度的18个网格单元的月降雨量数据,并开发了1925-1998年期间ENSO,PDO和当地SST的统计指标。我们发现ENSO减少了印度南部的降水,但对印度大部分地区的影响却很小。 PDO似乎放大了印度南部的ENSO信号,而当地的SST与南部半岛地区的季风降水总量直接相关。尽管这些关联在统计上通常很显着,但ENSO,PDO和SST的组合解释了整个印度季风降水变化的不足20%。 [参考:39]

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