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Raman lidar calibration for the DMSP SSM/T-2 microwave water vapor sensor

机译:DMSP SSM / T-2微波水蒸气传感器的拉曼激光雷达校准

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Campaigns were conducted at the Pacific Missile Range Facility, Barking Sands, Kauai, investigating Raman lidar as a method to improve calibration of the DMSP SSM/T-2 microwave water vapor profiling instrument. Lidar mixing ratios were calibrated against AIR and Vaisala radiosondes and the calibration was tested in the vicinity of clouds. Above 6 km, radiosondes reported anomalously low relative humidity in the vicinity of clouds. Lidar measurements were confirmed by using an electro-optical shutter, which provided correct measurement of relative humidity at cloud bases above 6 km. Radiative transfer calculations applied to the lidar data closely matched signals observed in the SSM/T-2 atmospheric channels. Forward calculations for surface sensitive channels disagreed with SSM/T-2 and SSM/I observations. Fine scale surface roughness and localized orographic drying are tentatively suggested as explanations. Cloud effects were ruled out as a significant source of discrepancy.
机译:运动在位于考艾岛Barking Sands的太平洋导弹靶场设施上进行,研究拉曼激光雷达,作为改善DMSP SSM / T-2微波水蒸气轮廓分析仪校准的方法。激光雷达混合比针对AIR和Vaisala无线电探空仪进行校准,并在云层附近进行校准。在6公里以上,无线电探空仪报告说云层附近的相对湿度异常低。激光雷达的测量通过使用光电快门确认,该快门可以正确测量6 km以上云层的相对湿度。应用于激光雷达数据的辐射传输计算与在SSM / T-2大气通道中观测到的信号非常匹配。对表面敏感通道的前向计算与SSM / T-2和SSM / I观测结果不一致。初步建议使用细尺度的表面粗糙度和局部地形干燥。排除了云效应是造成差异的重要原因。

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