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Monitoring of melting refreezing cycles of snow with microwave radiometers: the Microwave Alpine Snow Melting Experiment (MASMEx 2002-2003)

机译:用微波辐射计监测雪融化的再冻循环:微波高山融雪实验(MASMEx 2002-2003)

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A study of the melting cycle of snow was carried out by using ground-based microwave radiometers, which operated continuously 24 h/day from late March to mid-May in 2002 and from mid-February to early May in 2003. The experiment took place on the eastern Italian Alps and included micrometeorological and conventional snow measurements as well. The measurements confirmed the high sensitivity of microwave emission at 19 and 37 GHz to the melting-refreezing cycles of snow. Moreover, micrometeorological data made it possible to simulate snow density, temperature, and liquid water content through a hydrological snowpack model and provided additional insight into these processes. Simulations obtained with a two-layer electromagnetic model based on the strong fluctuation theory and driven by the output of the hydrological snowpack model were consistent with experimental data and allowed interpretation of both variation in microwave emission during the melting and refreezing phases and in discerning the contributions of the upper and lower layers of snow as well as of the underlying ground surface.
机译:使用地面微波辐射计对雪的融化周期进行了研究,该辐射计从2002年3月下旬至5月中旬和2003年2月中旬至5月初连续24小时/天运行。在意大利东部阿尔卑斯山,还包括微气象和常规降雪测量。这些测量结果证实了在19 GHz和37 GHz的微波发射对雪的融化-再冻循环具有很高的敏感性。此外,微气象数据使通过水文积雪模型模拟积雪密度,温度和液态水含量成为可能,并提供了对这些过程的更多见解。利用基于强波动理论的两层电磁模型进行的模拟,并由水文积雪模型的输出驱动,与实验数据一致,可以解释融化和再冻结阶段微波发射的变化,并可以分辨出贡献雪的上下两层以及下面的地面。

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