桑巴沿海站雨滴大小分布的季节变化

S. Lavanya, N. Kiran Kumar
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摘要

利用Joss-Waldvogel disdrometer在Thumba(8.5°N, 76.9°E)进行的长期(2007-2014)测量,研究了雨滴大小分布(DSD)的变化。东北季候风和西南季候风的DSD明显不同。结果表明,季风降水的日变化在大振幅降水的日变化模式上存在显著差异,在季风前和季风后两季均存在较弱的日变化,在夜间(19:00 LT)至午夜(04:00 LT)出现峰值。所有季节的降雨概率在东部时间10:00 - 13:00之间最小。DSD参数Dm(质量加权平均直径)的日变化也表现出明显的变化规律,与季风前和季风后相比,DSD参数Dm的值更小。在季风季节,由于大量小雨滴的存在,使Dm值降低。而在季风后和季风前,小雨滴较少,大雨滴较多,增加了Dm值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seasonal variations of raindrop size distribution over a coastal station Thumba
Variation of raindrop size distribution (DSD) are investigated using long-term (2007-2014) measurements made at Thumba (8.5°N, 76.9°E) by Joss-Waldvogel disdrometer. The DSD is observed to be distinctly different for NE and SW monsoon seasons. Results show a significant difference in the diurnal pattern of rainfall with large amplitude in the diurnal variation of rainfall in the monsoon with an evening (19:00 LT) to midnight (04:00 LT) peak and a weak diurnal variation in the Pre-monsoon and Post monsoon seasons. Probability of occurrence of rain is minimum during 10:00 – 13:00 LT for all seasons. The diurnal variation of DSD parameter Dm (mass-weighted mean diameter) also shows a distinct pattern with smaller values in monsoon compared to pre-, and post monsoon seasons. During monsoon season due to the presence of large number of small drops reduces the Dm value. While the presence of fewer small drops and relatively more big drops in the post and pre monsoon increases the values of Dm.
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