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Retrieval of Low-Level Marine Cloud Parameters from Airborne Observation Data

机译:从机载观测数据中检索低层海洋云参数

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摘要

研究概要:It is of great interest to investigate the radiative properties on the cloud optical, microphysical, and geometrical parameters, in particular, of low-level marine clouds which play crucial influence on a global climate system. Top height, base height, and geometrical thickness of cloud layer are considered here as cloud geometrical parameters. These parameters are very important because top and base heights are the factors which govern the strength of greenhouse effect through the thermal radiation from/to cloud layer, whereas the geometrical thickness is the key parameter for the estimation of gaseous absorption in cloud layer where multiple scattering process dominates. Some studies have shown that information of a few spectral regions including oxygen A band, enabled us possible to retrieve the cloud geometrical parameters as well as the optical thickness, the effective particle radius of cloud. In this study, an algorithm has developed to retrieve simultaneously the cloud optical thickness, effective particle radius, top height, and geometrical thickness of cloud layer from the spectral information of visible, near infrared, thermal infrared, and oxygen A band channels. This algorithm was applied to the actual airborne data which included the above four channels and targeted at the low-level marine clouds off the coast of California in summer. The retrieved results seems to be almost consistent to the in situ microphysical observation although further validation studies are required for the cloud geometrical parameters in particular.
机译:研究概要:研究云的光学,微物理和几何参数,特别是对全球气候系统起关键作用的低层海洋云的辐射特性,具有极大的兴趣。云层的顶部高度,基部高度和几何厚度在此处视为云几何参数。这些参数非常重要,因为顶部和底部的高度是决定通过/来自云层的热辐射来控制温室效应强度的因素,而几何厚度是估算多重散射的云层中气体吸收的关键参数。过程占主导地位。一些研究表明,包括氧气A带在内的几个光谱区域的信息使我们能够检索云的几何参数以及光学厚度,云的有效粒子半径。在这项研究中,开发了一种算法,可从可见,近红外,热红外和氧气A波段通道的光谱信息中同时检索云层的光学厚度,有效粒子半径,顶部高度和几何厚度。将该算法应用于实际的机载数据,其中包括上述四个通道,并且针对夏季加利福尼亚州沿海的低层海洋云。尽管特别是对于云的几何参数,还需要进一步的验证研究,但所获得的结果似乎与原位微物理观测几乎一致。

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