首页> 外文会议>Geoscience and Remote Sensing Symposium, 1995. IGARSS '95. 'Quantitative Remote Sensing for Science and Applications', International >In situ backscattering measurements of snowcover with coherent scatterometers at 5.3 and 35 GHz
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In situ backscattering measurements of snowcover with coherent scatterometers at 5.3 and 35 GHz

机译:使用相干散射仪在5.3和35 GHz下对积雪进行原位反向散射测量

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This paper presents backscattering measurements of snowcover with two scatterometers at 5.3 GHz (C-band) and 35 GHz (Ka-band). The data were recorded in the Swiss Alps on February 21 and 22, 1995 during stable, dry-snow conditions. The snow height varied from 1.25 to 1.40 m. Scattering profiles, the angular and spectral dependence of the backscattering coefficient /spl gamma/ and the amplitude of the correlation coefficient /spl rho/ at 5.3 GHz are shown. The authors found that the waves at C-band are mainly backscattered by the ground for incidence angles greater than 20/spl deg/. At 35 GHz, the backscattering originates from within the snowcover.
机译:本文介绍了使用两个散射仪在5.3 GHz(C波段)和35 GHz(Ka波段)对积雪进行反向散射测量。数据记录于1995年2月21日至22日在瑞士阿尔卑斯山稳定,干燥的雪况下。雪高从1.25到1.40 m不等。显示了在5.3 GHz时的散射曲线,后向散射系数/ spl gamma /的角度和光谱依赖性以及相关系数/ spl rho /的幅度。作者发现,对于入射角大于20 / spl deg /的情况,C波段的波主要被地面反向散射。在35 GHz时,后向散射起源于积雪内部。

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