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Atmospheric moisture measurements: a microwave radiometer-radiosonde comparison

机译:大气湿度测量:微波辐射计-探空仪比较

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摘要

The NASA/Goddard Space Flight Center Crustal Dynamics Project microwave Water Vapor Radiometer (WVR-J03) is used to measure the thermal emission of the sky at three frequencies (20.7, 22.2, and 31.4 GHz). Measurements were taken during the Atmospheric Moisture Intercomparison Study (ATMIS) held at Wallops Island, VA during April 1989. These measurements were compared with brightness temperatures inferred from measurements from VAISALA radiosonde packages launched every 3 h during the experiment period. An error analysis for the radiosonde-inferred brightness temperatures was performed, assuming reasonable random uncertainties for the pressure, temperature, and humidity measurements and propagating these uncertainties through the analysis algorithm. Two different water vapor emission models were used for the derivation of the brightness temperatures from the radiosonde measurements. Differences between the two models increase as the moisture content increases and vary as a function of frequency.
机译:NASA /哥达德太空飞行中心地壳动力学项目微波水蒸气辐射计(WVR-J03)用于测量三个频率(20.7、22.2和31.4 GHz)上天空的热辐射。在1989年4月于弗吉尼亚州瓦洛普斯岛举行的大气水分比对研究(ATMIS)中进行了测量。将这些测量结果与实验期间每3小时发射的VAISALA无线电探空仪包装的测量结果推算出的亮度温度进行了比较。对无线电探空仪推断的亮度温度进行了误差分析,假设压力,温度和湿度测量值具有合理的随机不确定性,并通过分析算法传播这些不确定性。两种不同的水蒸气排放模型用于从探空仪测量中推导出亮温度。两种模型之间的差异随着水分含量的增加而增加,并随频率而变化。

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