首页> 外文期刊>Mausam: Journal of the Meteorological Department of India >Rain drop size distribution characteristics of cyclonic and north east monsoon thunderstorm precipitating clouds observed over Kadapa (14.47°N, 78.82°E), Tropical semi-arid region of India
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Rain drop size distribution characteristics of cyclonic and north east monsoon thunderstorm precipitating clouds observed over Kadapa (14.47°N, 78.82°E), Tropical semi-arid region of India

机译:印度热带半干旱地区卡达帕(14.47°N,78.82°E)上空观测到的气旋和东北季风雷暴雨云的雨滴大小分布特征

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摘要

Raindrop size distributions (RSD) of "JAL" Cyclone induced precipitating clouds (7 Nov. 2010) and North- East (NE) monsoon thunderstorm precipitating clouds (16 November 2010) were measured with a Particle Size and Velocity (PARSIVEL) disdrometer deployed at Kadapa (14.47°N; 78.82°E), a semiarid continental site in Andhra Pradesh state, India. From the observational results we find that stratiform precipitation is predominant than convective precipitation in cyclone induced precipitation clouds. Where as in the case of NE monsoon thunderstorm precipitation convective cloud fraction is more than stratiform clouds. The cyclone induced precipitation is associated with higher concentration of small drops (small and middrops) in stratiform region (convective region) than NE monsoon precipitation. The average mass weighted diameter, Dm of cyclone induced precipitation is less than the NE monsoon precipitation both in stratiform and convective cloud regions. The observed RSD are found distinctly vary from cyclonic and NE monsoon thunderstorm precipitating clouds.
机译:使用部署在地面的“粒子大小和速度”(PARSIVEL)测风仪测量了“ JAL”旋风诱发的降水云(2010年11月7日)和东北(东北)季风雷暴降水云(2010年11月16日)的雨滴大小分布(RSD)。 Kadapa(北纬14.47°;东经78.82°),是印度安得拉邦的半干旱大陆站点。从观测结果我们发现,在旋风引起的降水云中,层状降水比对流降水为主。与NE季风雷暴一样,对流云比层状云要多。旋风诱导的降水与层状区域(对流区域)中的小滴(小和中滴)浓度高于东北季风降水有关。在层状云区和对流云区,气旋诱发降水的平均质量加权直径Dm小于NE季风降水。发现观测到的RSD与气旋和NE季风雷暴降水云明显不同。

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