赣南秋冬季降水云系特征综合探测试验

An Integrated Experiment of Precipitation Cloud Characteristic During Autumn-Winter in Southern Jiangxi

  • 摘要: 2015年10—12月对赣南地区降水云特征进行了综合试验,对观测数据集进行了对比,对降水云的分布特征进行了初步分析。观测资料比对结果表明:微波辐射计反演的温度和绝对湿度,可作为高时间分辨资料使用;雷达回波可用来反演雨粒子有效直径,在尚无更好资料的时候,也可作为参考用来反演云粒子有效直径。降水云特征初步分析表明:①赣南秋冬季(10—12月),降水云系云顶较高平均高度达8000 m,云层较厚平均厚度达5000 m以上;②雷达反演的云有效粒子直径的大小和垂直分布,可在一定程度上反映云系分布特征,平均云有效粒子直径大于30 um,厚度达3000 m,对产生降水有指示意义。

     

    Abstract: An integrated experiment of precipitation cloud characteristic in Southern Jiangxi from October to December 2015 carried out the comparison of observation data set and the distribution characteristic analysis for precipitation clouds. The comparison analysis of observation data set shows that: the temperature and absolute humidity retrieved by microwave radiometer can be used as high time resolution data set, the radar echoes can be used to retrieve the effective diameter of rain particles, and can also be used as a reference to retrieve the effective diameter of cloud particles when no better data set is available. The preliminary analysis of precipitation cloud characteristic shows that: (1) During October-December 2015 in southern Jiangxi, the precipitation clouds has a higher cloud top with an average height of 8000 m and a thicker cloud with an average thickness of more than 5000 m. (2) The size and vertical distribution of cloud effective particle diameters retrieved by radar, can reflect the distribution of the cloud characteristics to a certain extent. When the average effective particles diameter of cloud is greater than 30 μm and the thickness is up to 3000 m, which has indicative significance to produce precipitation.

     

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