首页> 外文期刊>Journal of Applied Remote Sensing >Optical properties of cirrus clouds at a tropical Indian station Gadanki, Tirupati (13.5 deg N, 79.2 deg E)
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Optical properties of cirrus clouds at a tropical Indian station Gadanki, Tirupati (13.5 deg N, 79.2 deg E)

机译:卷云的光学特性在蒂鲁伯蒂加丹基热带印度站(北纬13.5度,东经79.2度)

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The optical properties of the cirrus clouds over a tropical inland station Gadanki, Tirupati were studied using a dual polarization lidar. The extinction coefficient, backscatter coefficient, optical depth and linear depolarization of the cirrus clouds are derived using the range dependent lidar ratio. This work reports the results obtained during the period of December 2006 to July 2007 which covers the three prominent seasons of the year in the Indian subcontinent. A variety of ice crystals like hexagonal thin plate, thick plate, columns, dendrites and aggregates were observed within the cloud. The geometrical and optical thicknesses of the clouds show strong seasonal variations. The occurrence frequency of thin cirrus clouds was found to be relatively high as compared to sub-visible and dense clouds. In almost all the cases, the cloud contains smaller ice crystals in the top part, larger crystals in the middle portion and mixed phase in the bottom portion. Compared to the winter and summer seasons the horizontally oriented ice crystals were observed more in monsoon period. The lidar ratio and linear depolarization ratio of the cirrus clouds were in the range of 3-40 sr and 0.1-1.5 respectively. The maximum linear depolarization ratio was observed for the clouds containing randomly oriented ice crystal with temperature below -80~(0) C. The lidar ratio was found to be maximum for the thin plate crystals and minimum for thick clouds with horizontally oriented ice crystals. The extinction and backscattering coefficients of the clouds were in the range of 0.3X10~(-4) to 6X10~(-4) m~(-1) and 0.12X10~(-4) to 3X10~(-4) m~(-1) sr~(-1) respectively during the observation period.
机译:使用双偏振激光雷达研究了热带内陆台地加鲁日(Tirupati)上的卷云的光学特性。卷积云的消光系数,后向散射系数,光学深度和线性去极化是使用与距离有关的激光雷达比率得出的。这项工作报告了在2006年12月至2007年7月期间获得的结果,这些结果涵盖了印度次大陆一年中的三个突出季节。在云中观察到各种冰晶,如六角形薄板,厚板,圆柱,枝晶和聚集体。云的几何和光学厚度显示出强烈的季节性变化。发现薄卷云的发生频率与亚可见云和致密云相比较高。在几乎所有情况下,云层的顶部都包含较小的冰晶,中部包含较大的冰晶,而底部则包含混合相。与冬季和夏季相比,在季风期更多地观察到了水平定向的冰晶。卷云的激光雷达比和线性去极化比分别在3-40 sr和0.1-1.5的范围内。在温度低于-80〜(0)C的情况下,观察到包含随机取向的冰晶的云的最大线性去极化率。对于薄板状晶体,激光雷达的比率最大,而在水平取向的冰晶的情况下,激光雷达的激光雷达的最小值最小。云的消光和后向散射系数在0.3X10〜(-4)至6X10〜(-4)m〜(-1)和0.12X10〜(-4)至3X10〜(-4)m〜的范围内(-1)sr〜(-1)在观察期间。

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