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Cloud microphysical properties over Indian monsoon regions during CAIPEEX-2009

机译:CAIPEEX-2009期间印度季风区的云微物理性质

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Cloud microphysical data collected from an instrumented aircraft in the Cloud Aerosol Interaction and Precipitation Enhancement Experiment (CAIPEEX-2009) during May-September 2009 have been used to examine the nature of cloud drop size distributions (DSD), cloud drop effective radius (R _E) and their height variations at different locations during tropical Indian monsoons. Single mode drop size distributions were observed over Pathankot, Hyderabad and Bengaluru regions and bimodal DSD were recorded often over Guwahati and Bareilly regions. DSD spectral width showed height variation, being narrow at lower heights and broadening with increasing height. DSD spectra were narrow even at higher levels over Pathankot during pre-monsoon season and were very broad at Bareilly and Guwahati during the active phase of monsoon. The total concentrations of cloud droplets and percentage contribution of cloud droplet of radii≤10μm (small) and >10μm (large) showed interesting height variations and were different over different regions. The R _E showed nearly linear increases with height over all the regions. However, the droplet growth rate is observed to be different over different regions, being less over north (Bareilly and Pathankot: 1.3-1.46μm/km), intermediate over central (Hyderabad: 1.74μm/km) and highest over northeast (Guwahati: 1.92μm/km) and south (Bengaluru: 1.99μm/km) India.For the first time an attempt has been made to collect and explore cloud microphysical characteristics using in-situ aircraft observations during Indian monsoon conditions.
机译:在2009年5月至9月的“云气溶胶相互作用和降水增强实验(CAIPEEX-2009)”中,从一架仪器飞机收集的云微物理数据已用于检验云滴大小分布(DSD),云滴有效半径(R _E)的性质。 )及其在热带印度季风期间在不同位置的高度变化。在Pathankot,海得拉巴和班加罗尔地区观察到单模液滴尺寸分布,在Guwahati和Bareilly地区经常记录双峰DSD。 DSD光谱宽度显示出高度变化,在较低高度处变窄,并随高度增加而变宽。在季风前季节,Pathankot的DSD光谱即使在较高水平也很窄,而在季风活跃期的Bareilly和Guwahati则非常宽。半径≤10μm(小)和>10μm(大)的云滴的总浓度和云滴的百分比贡献显示出有趣的高度变化,并且在不同区域之间存在差异。 R _E在所有区域都显示出随着高度的增加几乎呈线性增长。然而,在不同地区观察到的液滴生长速率有所不同,在北部(Bareilly和Pathankot:1.3-1.46μm/ km)较小,在中部(海得拉巴:1.74μm/ km)中等,在东北部(Guwahati:印度南部(孟加拉国:1.99μm/ km)(1.92μm/ km)。第一次尝试通过印度季风条件下的飞机实地观测来收集和探索云的微物理特征。

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