首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Pre-monsoon/monsoon thunderstorm characteristics over Pune-An investigation using Doppler Sodar observations
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Pre-monsoon/monsoon thunderstorm characteristics over Pune-An investigation using Doppler Sodar observations

机译:浦那季风前/季风雷暴特征-使用多普勒·索达尔观测资料进行的调查

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摘要

Doppler sodar observations of three dimensional (3D) wind fields and thermal structure of convective boundary layer (CBL) on a few thunderstorm days of 2009 during pre-monsoon (May and June; June due to delayed arrival of monsoon over Pune) and monsoon (July and August) are analyzed. They reveal the typical signatures of wind fields for the late afternoon thunderstorm (TS) such as deceleration of winds with or without change in direction leading to convergence a few minutes (~15-30. min) prior to the onset of TS. Pre-monsoon TS are characterized by broad updrafts and narrow downdrafts in CBL in contrast to the narrow updrafts and broad downdrafts of a normal day (i.e. No-TS day). Mean vertical velocity averaged over CBL period shows net updraft on TS days and net downdraft on No-TS day for the pre-monsoon cases. Similarly calm winds are observed in the CBL on TS-days that support enhanced free convection. During the monsoon period updrafts are observed on both TS and No-TS days with higher values on TS days in comparison, due to the dominance of large-scale monsoon flow over local convection. Relatively higher turbulence kinetic energy (TKE) in CBL is observed on all TS days. Analysis shows that TKE maximum for the day is attained about 1.5-2.0. h prior to the onset of afternoon TS. Mixed-layer depth, determined from TKE profile, is higher than lifting condensation level (LCL) on TS days in May and June indicating saturation of air parcels in updrafts.
机译:在季风前期(5月和6月; 6月,由于季风在浦那到达较晚)和季风( 7月和8月)进行了分析。它们揭示了午后雷暴(TS)的典型风场特征,例如风向的减速(有或没有变化),导致在TS发作前几分钟(约15-30分钟)收敛。季风前TS的特征是CBL的上升气流和下降气流窄,而正常日(即非TS天)的上升气流和下降气流窄。在季风前的情况下,CBL期间的平均垂直速度平均在TS天呈净上升趋势,在No-TS天呈净下降趋势。同样,在TS天,CBL中观察到平静的风,支持增强的自由对流。在季风期间,由于大季风流量在局部对流中占主导地位,因此在TS和No-TS日均观测到上升气流,而在TS日上观测到更高的值。在所有TS天中,在CBL中观察到相对较高的湍流动能(TKE)。分析表明,当天的TKE最大值约为1.5-2.0。在下午TS发作之前的h。由TKE剖面确定的混合层深度高于5月和6月TS日的抬升凝结水位(LCL),表明上升气流中的空气包裹已饱和。

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