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Passive Millimeter-wave Signatures of Ice Particles in Hurricane Erin

机译:艾琳飓风中冰粒的被动毫米波特征

摘要

Observations of Hurricane Erin (2001) taken during the Fourth Convection and Moisture Experiment (CAMEX-Q) are used to elucidate relationships between measurements and models. Measurements include active and passive microwave sensors, and dropsondes. Models used in the analysis include radiative transfer (RT) models, mesoscale models (MM5), and particle parameterizations. Various combinations of the models and observational constraints are used in the RT model to provide calculated brightness temperatures to compare to the passive observations. In order to match the wide frequency range 10 to 183+/-10 GHg model modifications were needed. The 55.5 GHz channel provided insight to the tropospheric temperature profile, while the 10 GHz channel provided knowledge of (near) ocean surface conditions. The channels less than approx.90 GHz are mostly responsive to liquid in the cloud, while higher frequencies respond to ice particles in the cloud. Keywords-ice clouds, precipitation, millimeter-wave, retrievals.
机译:在第四次对流和水分实验(CAMEX-Q)中对艾琳飓风(2001)的观测结果被用来阐明测量值与模型之间的关系。测量包括有源和无源微波传感器以及探空仪。分析中使用的模型包括辐射传输(RT)模型,中尺度模型(MM5)和粒子参数化。在RT模型中使用模型和观测约束的各种组合来提供计算的亮度温度,以与被动观测进行比较。为了匹配较宽的频率范围,需要对10至183 +/- 10 GHg的模型进行修改。 55.5 GHz信道提供了对流层温度剖面的洞察力,而10 GHz信道提供了(近)海洋表面状况的知识。小于约90 GHz的信道主要对云中的液体做出响应,而更高的频率对云中的冰粒做出响应。关键字:冰云,降水,毫米波,取回。

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