水晶脸期间用紧凑扫描亚毫米成像辐射计和云雷达系统的冰云检索与分析

K. F. Evans, James R. Wang, P. Racette, G. Heymsfield, Lihua Li
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引用次数: 95

摘要

摘要亚毫米波辐射测量是一种测量对流层上层冰云中冰路径和冰云颗粒大小的新技术。2002年7月,在“热带卷云和卷云层的卷云区域研究”(CRYSTAL)佛罗里达地区卷云实验(FACE)活动期间,使用紧凑型扫描亚毫米成像辐射计(CoSSIR)测量了340 GHz以上冰云的首批亮度温度图像。CoSSIR在183、220、380、487和640 GHz的接收器上运行12个频道。CoSSIR和最低点观测94 ghz云雷达系统(CRS)在NASA的ER-2飞机上飞行,该飞机位于佛罗里达州的基韦斯特。对CoSSIR亮度温度的定性比较表明,亚毫米波频率对铁砧冰云粒子比低频频率更敏感。采用贝叶斯算法,结合原位云探测器的先验微物理信息,反演了IWP和中位质量等效球颗粒直径(Dme)。麦克风……
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Ice Cloud Retrievals and Analysis with the Compact Scanning Submillimeter Imaging Radiometer and the Cloud Radar System during CRYSTAL FACE
Abstract Submillimeter-wave radiometry is a new technique for determining ice water path (IWP) and particle size in upper-tropospheric ice clouds. The first brightness temperatures images of ice clouds above 340 GHz were measured by the Compact Scanning Submillimeter Imaging Radiometer (CoSSIR) during the Cirrus Regional Study of Tropical Anvils and Cirrus Layers (CRYSTAL) Florida Area Cirrus Experiment (FACE) campaign in July 2002. CoSSIR operated with 12 channels from receivers at 183, 220, 380, 487, and 640 GHz. CoSSIR and the nadir-viewing 94-GHz Cloud Radar System (CRS) flew on the NASA ER-2 airplane based out of Key West, Florida. A qualitative comparison of the CoSSIR brightness temperatures demonstrates that the submillimeter-wave frequencies are more sensitive to anvil ice cloud particles than are the lower frequencies. A Bayesian algorithm, with a priori microphysical information from in situ cloud probes, is used to retrieve the IWP and median mass equivalent sphere particle diameter (Dme). Mic...
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