2013年印度洋异常气旋形成的环境能量学特征

S. Dutta, S. Narkhedkar, S. Devi, S. Tm
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引用次数: 0

摘要

从大气能量学的角度,试图了解2013年气旋季节印度洋上异常气旋形成背后的动力学。本研究结果的显著特征是:所有强气旋涡的最大强度增强都与涡有效势能向涡动能(AE到KE)和纬向动能向涡动能(KZ到KE)的转换增强有关。•在风暴增强期间,声发射和AZ都被消散,表明风暴的增强是以声发射和AZ为代价的。•对于所有这些系统,斜压涡动能转换[从AE到KE的转换]比正压涡动能转换[从KZ到KE的转换]占主导地位。·2013年的异常气旋形成,至少部分可能归因于环境湿静态能(MSE)的正异常以及研究区域气旋季节斜压和正压涡旋动能转换的正异常。大气中对流不稳定性的释放也可归因于,至少部分归因于2013年的异常气旋形成。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Environmental Energetics aspects of anomalous Cyclogenesis over Indian Ocean during 2013
An attempt has been made to understand the dynamics behind anomalous cyclogenesis over Indian Ocean during 2013 cyclone seasons, from an atmospheric energetics point of view. Salient features of the results of this study are:Maximum intensification of all the intense cyclonic vortices was associated with an enhancement in both conversion from eddy available potential energy to eddy kinetic energy (AE to KE ) and zonal kinetic energy to eddy kinetic energy (KZ to KE).During intensification of the storms both AE and AZ have shown to be dissipated, suggesting the intensification of storms at the cost of AE and AZ . For all of these systems baroclinic eddy kinetic energy conversions [conversion from AE to KE ] dominates over barotropic eddy kinetic energy conversions [conversion from KZ to KE]. Anomalous cyclogenesis in 2013, at least partly may be attributed to a positive anomaly in Moist Static Energy (MSE) of the environment along with positive anomaly in baroclinic and barotropic eddy kinetic energy conversion during cyclone seasons over the region under study.Release of convective instability in the atmosphere may also be attributed, at least partly, for anomalous cyclogenesis in 2013.
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