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Tundra Snow Emissivities at MHS Frequencies: MEMLS Validation Using Airborne Microwave Data Measured During CLPX-II

机译:MHS频率处的苔原雪发射率:使用在CLPX-II期间测量的机载微波数据进行的MEMLS验证

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Presented within this paper is an analysis of data from five flights of the Facility for Airborne Atmospheric Measurement BAe146 during the February 2008 Cold Land Processes II campaign over the North Slope of Alaska. Snow pits were dug under the aircraft tracks which provided information about snow pack stratigraphy and grain type, density, and temperature profiles. Lambertian emissivity retrievals were carried out yielding an emissivity and effective temperature time series for each of the five flights discussed. These emissivities were used as the truth for the validation of the Microwave Emission Model of Layered Snowpacks (MEMLS) appropriate for use at Microwave Humidity Sounder and Advanced Microwave Sounding Unit B frequencies. As there are uncertainties in the model input parameters which were determined from the snow pit measurements, an efficient global optimization routine was used to determine if MEMLS could adequately simulate the observed emissivities within the uncertainties of the input parameters. In order to reduce model errors, various optimization experiments were carried out. The most successful of these were obtained in the following two cases: 1) A parameterization of surface roughness was introduced, and 2) a limit on the scattering coefficient at high frequency was introduced. In both of these cases, MEMLS is able to reproduce the emissivity spectra over the sites studied within the uncertainties in the measurements.
机译:本文介绍的是对2008年2月在阿拉斯加北坡进行的冷陆过程II战役中机载大气测量设施BAe146的五次飞行数据的分析。在飞机航迹下挖了雪坑,这些雪坑提供了有关积雪地层,颗粒类型,密度和温度剖面的信息。进行了朗伯辐射率检索,得出了所讨论的五个飞行中的每一个的辐射率和有效温度时间序列。这些发射率被用作验证适用于微波湿度探测器和高级微波探测单元B频率的分层积雪的微波发射模型(MEMLS)的真相。由于从雪坑测量确定的模型输入参数中存在不确定性,因此使用有效的全局优化例程来确定MEMLS是否可以在输入参数的不确定性内充分模拟观察到的发射率。为了减少模型误差,进行了各种优化实验。其中最成功的方法是在以下两种情况下进行的:1)对表面粗糙度进行参数化,2)对高频散射系数进行限制。在这两种情况下,MEMLS都能在测量的不确定性范围内在所研究的位置上再现发射光谱。

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