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首页> 外文期刊>Theoretical and applied climatology >Impact of Indian Ocean warming on increasing trend in pre-monsoon rainfall and Hadley circulation over Bay of Bengal
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Impact of Indian Ocean warming on increasing trend in pre-monsoon rainfall and Hadley circulation over Bay of Bengal

机译:印度洋变暖对孟加拉湾季风降雨和Hadley循环的增加趋势

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摘要

In the present manuscript, we analyzed the pre-monsoon (March-April-May) rainfall over the Indian summer monsoon region using the Global Precipitation Climatology Project (GPCP) rainfall datasets during 1979-2015. It is found that the rainfall over the Bay of Bengal (BOB) has increased significantly and it is associated with the strengthening of local Hadley circulation over the BOB. The increasing Sea Surface Temperature (SST) over the Indian Ocean is playing an important role to the observed changes in convections and cloudiness over the BOB. In addition, the strengthening of the westerly enhances the wind speed and transports more moisture to the North Indian Ocean. In addition, warming of the SST and large-scale moisture convergence cause the rainfall to increase and the latent heat released in the process strengthens the divergent wind at 200hPa. This strengthens the local Hadley circulation over the BOB, which may affect the monsoon strength over the Indian subcontinent, by influencing the onset of the Indian summer monsoon. This study will improve the understanding by monitoring the changes in the atmospheric processes over the BOB and the Indian subcontinent, which may result in better predictability of the Indian summer monsoon.
机译:在目前的稿件中,我们在1979 - 2015年期间使用全球降水降雨量项目(GPCP)降雨数据集进行了印度夏季季风地区的季风普通话(3月至4月至5月)降雨。发现孟加拉湾(BOB)的降雨量显着增加,并且它与加强鲍勃的局部哈德利循环有关。在印度洋上增加海面温度(SST)正在为观察到的对流变化和鲍勃浑浊的变化发挥着重要作用。此外,加强西方增强风速,向北印度洋运输更多的水分。此外,SST和大规模水分收敛的热化导致降雨量增加,而且该过程中释放的潜热增强了200HPa的发散风。这通过影响印度夏季季风的发作,加强了鲍勃上的当地哈德利循环,这可能会影响印度次大陆的季风强度。本研究将通过监测鲍勃和印度次大陆的大气流程的变化来改善理解,这可能导致印度夏季季风的更好可预测性。

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  • 来源
    《Theoretical and applied climatology》 |2019年第4期|2595-2606|共12页
  • 作者单位

    Chinese Acad Sci Inst Atmospher Phys Ctr Monsoon Syst Res 40 Hua Yan Li Beijing 100029 Peoples R China|Univ Chinese Acad Sci Beijing Peoples R China;

    Chinese Acad Sci Inst Atmospher Phys Ctr Monsoon Syst Res 40 Hua Yan Li Beijing 100029 Peoples R China;

    Chinese Acad Sci Inst Atmospher Phys Ctr Monsoon Syst Res 40 Hua Yan Li Beijing 100029 Peoples R China;

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