本文研究了2017年春季孟加拉灣小型暖池對(duì)熱帶氣旋Maarutha（4月14—17日）以及熱帶氣旋Mora（5月27—30日）的影響.利用衛(wèi)星遙感和現(xiàn)場(chǎng)觀測(cè)數(shù)據(jù)分析發(fā)現(xiàn),盡管春季孟加拉灣熱帶氣旋確實(shí)能引起海洋上層冷卻效應(yīng),但是其冷卻強(qiáng)度受到暖池強(qiáng)度的影響.本文進(jìn)一步對(duì)比孟加拉灣小型暖池對(duì)兩個(gè)熱帶氣旋的響應(yīng)情況,發(fā)現(xiàn)當(dāng)春季小型暖池的溫度大于31℃（熱帶氣旋Mora期間）,暖池效應(yīng)能有效抑制海洋上層混合層的加深,降低熱帶氣旋引起的潛熱通量損失帶來(lái)的冷卻效應(yīng),并在一定程度上加強(qiáng)了熱帶氣旋. 

【文章來(lái)源】：南京信息工程大學(xué)學(xué)報(bào)(自然科學(xué)版). 2020,12(04)

【文章頁(yè)數(shù)】：12 頁(yè)

【文章目錄】：
0 Introduction
1 Data and methodology
2 Results and discussion
    2.1 Formation of spring MWP in the BoB
    2.2 Tracks of TC Maarutha and TC Mora
    2.3 Atmospheric-oceanic conditions during TC Mora
    2.4 Effect of spring MWP on TCs in the BoB
3 Conclusion


【參考文獻(xiàn)】：
期刊論文
[1]Vortex genesis over the Bay of Bengal in spring and its role in the onset of the Asian Summer Monsoon[J]. WU GuoXiong1, GUAN Yue1,2, WANG TongMei3, LIU YiMin1, YAN JingHui4 & MAO JiangYu1 1 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; 2Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3Department of Atmospheric Science, Sun Yat-Sen University, Guangzhou 510275, China; 4National Climate Center, China Meteorological Administration, Beijing 100080, China.  Science China（Earth Sciences）. 2011(01)



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