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Teleconnections between the sea surface temperature in the Bay of Bengal and monsoon rainfall in Bangladesh

机译:孟加拉湾海表温度与孟加拉国季风降雨之间的遥相关

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摘要

To explore the teleconnection between sea surface temperature (SST) and summer monsoon rainfall in Bangladesh, this study examined 90 yrs (1912-2001) of monthly rainfall data for twelve stations for the months of May (pre-monsoon month), and June through September (monsoon months) and SST of the Bay of Bengal for the same time period at 2° by 2° grid cells. A significant positive correlation (0.64) was found between the All-Bangladesh Monsoon Rainfall (ABMR) and SST over the Bay of Bengal in the month of June. All other contemporaneous monthly correlations were not found to be significant. The SST over the Bay of Bengal was positively correlated with June rainfall at all coastal stations in Bangladesh, and significantly for the Comilla station. The prevailing wind has a south-easterly component at this station, due to deflection caused by the coastal hills. Thus, the orographic effect in the east and the north-eastern part of the country appears to enhance the rainfall amounts in that area. The SST over the Bay of Bengal is especially important at 89°, 93°, and 95° East longitudes for predicting the June rainfall in Bangladesh.
机译:为了探讨孟加拉国海表温度(SST)与夏季季风降雨之间的遥相关性,本研究调查了5月(季风前一个月)和6月至6月至9月的90年(1912-2001年)月度降雨数据。孟加拉湾的9月(季风月份)和SST处于2°x 2°网格单元的同一时间段。在6月的孟加拉湾全孟加拉季风雨量(ABMR)与SST之间发现显着正相关(0.64)。没有发现所有其他同期的月度相关性均显着。孟加拉湾的海表温度与孟加拉国所有沿海站的六月降水量呈正相关,而Comilla站则显着。由于沿海山丘引起的偏转,盛行的风在该站具有东南风分量。因此,该国东部和东北部的地形效应似乎增加了该地区的降雨量。在预测孟加拉国六月降雨量的东经89°,93°和95°处,孟加拉湾的海表温度尤为重要。

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