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Onset characteristics of the southwest monsoon over India

机译:印度西南季风的爆发特征

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Dynamic and thermodynamic characteristics of the Asian summer monsoon during the onset phase over the Indian Peninsula (Kerala coast) and its variability are examined with reanalysis data sets. For this study, daily averaged (0000 and 1200 UTC) reanalysis data sets of National Centre for Environmental Prediction-National Centre for Atmospheric Research for the period 1948-99 are used. Based on 52 years of onset dates of the Indian summer monsoon, we categorized pre-onset, onset and post-onset periods (each averaged 5 days) to investigate the mean circulation characteristics and the large-scale energetics of the Asian summer monsoon. It is found that the strength of the low-level Somali jet and upper tropospheric tropical easterly jet increase rapidly during the time of evolution of the summer monsoon over India. Over the Bay of Bengal and the Arabian Sea, predominant changes are noticed in the large-scale balances of kinetic energy, heat and moisture from the pre-onset to the post-onset periods. Prior to the onset of the summer monsoon over India, a zone of flux convergence of heat and moisture is noticed over the eastern sector of the Bay of Bengal and this intensifies in the onset and post-onset periods. During onset of the monsoon over India, the horizontal flux convergence of heat and moisture, as well as diabatic heating, are enhanced over the Arabian Sea. These subsequently increase with the evolution and advancement of the monsoon over India. Further, the dynamics of the evolution processes (15 days before and 30 days after the onset date of the monsoon over Kerala for each annual cycle) are studied over various sectors, such as the Arabian Sea, Bay of Bengal and Indian Peninsula region. The study reveals that the low-level kinetic energy, vertically integrated generation of kinetic energy and net tropospheric moisture over Arabian Sea can be used as potential predictors for the prediction of the possible onset date of the summer monsoon over the Indian Peninsula.
机译:通过重新分析数据集,研究了印度半岛(喀拉拉邦海岸)爆发期亚洲夏季风的动态和热力学特征及其变化​​。对于本研究,使用了国家环境预测中心-国家大气研究中心1948-99年期间的每日平均(0000和1200 UTC)再分析数据集。基于印度夏季风的52年发病日期,我们对发病前,发病和发病后时期(每个平均为5天)进行了分类,以研究亚洲夏季风的平均环流特征和大规模能量。研究发现,在印度夏季风的演变过程中,低空的索马里急流和对流层热带东风急流的强度迅速增加。在孟加拉湾和阿拉伯海上,从发病前到发病后期间,动能,热量和水分的大规模平衡都发生了显着变化。在印度夏季风爆发之前,在孟加拉湾东部地区发现了热量和水分通量收敛的区域,并且在发病期和发病后期加剧。在印度季风爆发期间,阿拉伯海上热量和水分的水平通量收敛以及非绝热加热都得到了增强。随着印度季风的发展和进步,这些增加。此外,还研究了阿拉伯海,孟加拉湾和印度半岛地区等各个部门的演化过程动力学(每个季节的喀拉拉邦季风爆发日期前15天和之后30天)。该研究表明,阿拉伯海上的低水平动能,垂直积分动能和对流层净水分可以用作预测印度半岛夏季季风可能发生日期的潜在预测因子。

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