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首页> 外文期刊>Geophysical Research Letters >Air-sea interaction over the Indian Ocean during the contrasting monsoon years 2002 and 2003 - art. no. L14821
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Air-sea interaction over the Indian Ocean during the contrasting monsoon years 2002 and 2003 - art. no. L14821

机译:在2002年和2003年不同的季风季节期间,印度洋上的海海互动-艺术。没有。 L14821

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摘要

The air-sea interaction processes over the Indian Ocean are studied using the satellite data from the Tropical Rainfall Measuring Mission Satellite for two contrasting monsoon years, namely 2002 ( deficit) and 2003 ( normal). The moisture transport for the two contrasting years was also analyzed using the NCEP/NCAR reanalysis data. Linear correlation coefficient between the convective heating over the Bay of Bengal and the zonal wind at 850 hPa over the peninsular India showed the maximum negative correlation ( - 0.41) and is statistically significant at 99.9% significance level with a lag of 3 days, with convection leading. The evaporation rates were lower ( higher) over the Arabian Sea during active ( weak) monsoon conditions, indicating its negligible influence on the ensuing monsoon activity over the subcontinent. Water vapor contents decreased substantially prior to the break over the Arabian Sea and low values prevailed throughout the break period. Further, it was seen that more moisture was transported into the subcontinent ( equatorial region) during the active ( weak) monsoon conditions.
机译:利用来自热带雨量测量任务卫星的卫星数据研究了两个截然不同的季风年,即2002年(赤字)和2003年(正常),研究了印度洋上的海-海相互作用过程。还使用NCEP / NCAR再分析数据分析了两个对比年份的水分传输。孟加拉湾对流加热和印度半岛上850 hPa纬向风之间的线性相关系数显示最大负相关(-0.41),在99.9%的显着性水平上具有统计学显着性,滞后3天,对流领导。在活跃的(弱)季风条件下,阿拉伯海的蒸发速率较低(较高),表明其对随后的次大陆上季风活动的影响可忽略不计。在突破阿拉伯海之前,水蒸气含量大幅下降,并且整个断裂期间的水汽含量普遍较低。此外,可以看出,在活跃的(弱)季风条件下,更多的水分被输送到次大陆(赤道地区)。

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