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Characterisation and asymmetry analysis of rainfall distribution associated with tropical cyclones over Bay of Bengal : NISHA (2008), LAILA (2010) and JAL (2010)

机译:孟加拉湾与热带气旋有关的降雨分布的特征和非对称性分析:NISHA(2008),LAILA(2010)和JAL(2010)

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摘要

The precipitation characteristics and spatial rainfall asymmetry in respect of three tropical cyclones (TCs) of Bay of Bengal, viz., NISHA (2008), LAILA (2010) and JAL(2010) that affected coastal Tamil Nadu are studied using TRMM based rain rate data. The analysis is carried out by dividing the life cycle of the TC into various stages of intensification and weakening. Percentage frequency distribution, radial profile and quadrant-wise mean rain rates are determined stage-wise for each TC. Further, spatio-temporal variations in the rainfall asymmetry is studied using Fourier analysis by computing the first order wave number-1 asymmetry around the TC centre. The results indicate a shifting of higher frequency rain rates from higher to lower rain rate side when the TC passes from intensification to weakening stages. The azimuthally averaged mean rain rates indicate a peak rain rate of 4-5 mm/hr over 50-100 km from the TC centre during intensification stages which decreases to a very low rate of about 1 mm/hr during the final stages of weakening. For the same intensity category, the radial profiles of mean rain rates show marked difference between the intensification and weakening stages. The quadrant mean rain rates show large asymmetries in the radial rainfall distribution with more rainfall concentrated in front left quadrant during the stages of intensification. Such TC rainfall asymmetries are shown to be influenced by the environmental vertical wind shear and translational speed of the TC. When the wind shear and storm motion vectors are in the same direction, a dominant down shear left asymmetry is observed. Evolution of wave number-1 asymmetry indicates that, by and large, asymmetry amplitude increases from the centre outwards and a cyclonic (anti-cyclonic) shift during the intensification (weakening) stages of the TCs.
机译:利用基于TRMM的降雨率研究了孟加拉湾的三个热带气旋(TCs),即NISHA(2008),LAILA(2010)和JAL(2010)对北部沿海泰米尔纳德邦的降水特征和空间降雨不对称性数据。通过将TC的生命周期分为强化和减弱的各个阶段进行分析。每个TC的阶段频率确定百分比频率分布,径向分布和象限方向平均降雨率。此外,通过计算TC中心周围的一阶波数不对称性,使用傅里叶分析研究了降雨不对称性的时空变化。结果表明,当热带气旋从强化阶段过渡到减弱阶段时,高频降雨率从较高降雨率侧向较低降雨率侧转移。方位角平均降雨率表示在强化阶段距TC中心50-100 km处的峰值降雨率为4-5 mm / hr,在减弱的最后阶段降低至约1 mm / hr的极低速率。对于相同强度的类别,平均降雨率的径向曲线显示出强化阶段和减弱阶段之间存在显着差异。象限平均降雨率在径流降雨分布中显示出较大的不对称性,在强化阶段,更多的降雨集中在左前象限。此类TC降雨的不对称性受环境垂直风切变和TC平移速度的影响。当风切变和风暴运动矢量在相同方向上时,观察到主要的向下切变左不对称性。 1号波不对称性的演变表明,在TC的增强(减弱)阶段,不对称振幅从中心向外大幅度增加,并且发生了气旋(反气旋)偏移。

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