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Comparison of atmospheric profiles between microwave radiometer retrievals and radiosonde soundings

机译:微波辐射计检索和探空仪探测之间的大气廓线比较

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Atmospheric profiles of temperature (T), vapor density (ρv), and relative humidity (RH) retrieved from ground-based microwave radiometer (MWR) measurements are compared with radiosonde soundings at Wuhan, China. The MWR retrievals were averaged in the ±30 min period centered at sounding times of 00 and 12 UTC. A total of 403 and 760 profiles under clear and cloudy skies were selected. Based on the comparisons, temperature profiles have better consistency than the ρv and RH profiles, lower levels are better than upper levels, and the cloudy are better than the clear-sky profiles. Three cloud types (low, middle, and high) were identified by matching the infrared radiation thermometer-detected cloud base temperature to the MWR-retrieved temperature-height profiles. Temperature profile under high cloud has the highest correlation coefficient (R) and the lowest bias and RMS, but under low cloud is in the opposite direction. The ρv profile under middle cloud has the highest R and the lowest bias but under high cloud has the lowest R, the largest bias, and RMS. Based on the radiosonde soundings, both clear and cloudy wind speeds and drifting distances increase with height but increase much faster under clear than cloudy above 4km. The increased wind speeds and drifting distances with height have resulted in decreased correlation coefficient and increased temperature biases and RMSs with height for both clear and cloudy skies. The differences in R, bias, and RMS between clear and cloudy skies are primarily resulted from their wind speeds and drifting distances.
机译:从地面微波辐射计(MWR)测量获得的温度(T),蒸气密度(ρv)和相对湿度(RH)的大气廓线与中国武汉的探空仪测深进行了比较。 MWR取回值在±30分钟内取平均值,以发声时间00和12 UTC为中心。在晴朗和多云的天空下,总共选择了403和760个剖面。根据比较,温度曲线比ρv和RH曲线具有更好的一致性,较低的水平优于较高的水平,而多云的天空优于晴天。通过将红外辐射温度计检测到的云底温度与MWR检索到的温度高度剖面进行匹配,可以识别出三种云类型(低,中和高)。高云下的温度分布具有最高的相关系数(R),最低偏置和RMS,但低云下的温度分布方向相反。中云下的ρv剖面具有最高的R和最低的偏差,而高云下的ρv剖面具有最低的R,最大的偏差和RMS。根据探空仪的探测,晴空和阴天的风速和漂移距离都随着高度的增加而增加,但晴空下的增长速度要快于4km以上的阴天。对于晴朗和多云的天空,随着高度的增加,风速和漂移距离会导致相关系数降低,并且随着高度的升高,温度偏差和均方根值也会增加。晴空之间的R,偏差和RMS的差异主要是由它们的风速和漂移距离引起的。

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