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Cloud droplet/particle sizes obtained from emitted radiances

机译:从发射辐射中获得的云滴/颗粒大小

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Abstract: Global scale satellite observations of cloud properties are a key to unraveling the physical processes that govern the role clouds play in the climate system. The retrieval of cloud particle size from satellite imagery data is of particular interest. Cloud emissivities and transmissivities depend substantially on the constituent single particle scattering and absorbing properties which in turn depend on particle size. Two clouds with the same ice water content but different particle sizes may have substantially different optical depths. This study presents a retrieval scheme for obtaining cloud droplet/particle size from satellite measurements at infrared wavelengths. The scheme employs Mie theory and the Eddington approximation and uses the advanced very high resolution radiometer (AVHRR) data at 3.7, 11, and 12 $mu@m. It also relies on the nonlinear relationships between 3.7, 11, and 12 $mu@m radiances observed for single- layered semitransparent cloud systems. Theory indicates that the nonlinear relationships disappear when the spherical particle radius reaches about 60 $mu@m. An automated retrieval procedure has been developed. Some retrieved results are presented. !2
机译:摘要:全球卫星对云的性质的观测是揭示控制云在气候系统中作用的物理过程的关键。从卫星图像数据中检索云的粒径特别令人感兴趣。云的发射率和透射率基本上取决于组成的单个颗粒的散射和吸收特性,而散射和吸收特性又取决于颗粒尺寸。冰水含量相同但粒径不同的两朵云可能具有实质上不同的光学深度。这项研究提出了一种从红外波长的卫星测量中获得云滴/粒径的检索方案。该方案采用Mie理论和Eddington近似,并使用先进的超高分辨率辐射计(AVHRR)数据,分别为3.7、11和12μm@ m。它还依赖于对单层半透明云系统观察到的3.7、11和12 $μm辐射之间的非线性关系。理论表明,当球形粒子半径达到约60μm@ m时,非线性关系消失。已经开发了一种自动检索程序。提出了一些检索结果。 !2

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