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Ocean atmospheric processes over Bay of Bengal during two contrasting northeast monsoon onsets
Indian Journal of Geo-Marine Sciences ( IF 0.5 ) Pub Date : 2020-11-05
K V Shende, M R Ramesh Kumar, K V Kale

Conditions leading at the beginning of North-East Monsoon season on the Bay of Bengal studied using various ocean/ atmosphere parameters such as wind speed, shortwave radiation, sea surface temperature, latent heat flux, net surface heat flux and outgoing longwave radiation for two contrasting North-East monsoon onset years such as 1984 (Delayed) and 1999 (Early). During 1984 sea surface temperature is high over the northern portion of the Bay of Bengal but in 1999 which is the early North-East Monsoon year it is high over the south-eastern portion. In the delayed year i.e. in 1984, sea surface temperature over northern portion of Bay of Bengal warms more than an earlier year i.e. 1999, but contrast behaviour is observed in the south-eastern portion, it warms more in 1999 than 1984. From the analysis, it also observed that in delayed year more heat evaporates than an early year.

中文翻译:

两次相反的东北季风爆发期间孟加拉湾的海洋大气过程

使用两个不同的海洋/大气参数,例如风速,短波辐射,海面温度,潜热通量,净表面热通量和外向长波辐射,研究了孟加拉湾东北季风季节开始时的领先条件。东北季风的爆发年份如1984年(延迟)和1999年(早期)。在1984年期间,孟加拉湾北部的海表温度较高,但在东北季风初期的1999年,其东南部的温度较高。在延迟的年份(即1984年),孟加拉湾北部的海表温度比早期的年份(即1999年)温暖,但在东南部观察到对比现象,1999年的温度比1984年高。 ,
更新日期:2020-11-06
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