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首页> 外文期刊>Geocarto international >Using cosmo-skymed images to detect wet snow cover on the Krakow Ice Field, King George Island, Antarctica
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Using cosmo-skymed images to detect wet snow cover on the Krakow Ice Field, King George Island, Antarctica

机译:使用cosmo-skymed图像来检测克拉科夫冰场,乔治岛,南极洲国王冰野的湿雪盖

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This work analysed the spatio-temporal variation of snow cover on the Krakow Ice Field, located in the King George Island, Antarctica. High spatial resolution images of COSMO-SkyMed were used in this study. These X-band images are vertically and horizontally co-polarized and their intensity data were converted to amplitude (dB). The COSMO-SkyMed images were classified by a minimum distance algorithm and post-classified based on knowledge of adjacency relationships of snow zones. Hypsometric, slope, aspect and solar radiation maps to support the interpretation of backscatter patterns in the COSMO-SkyMed images. Three radar zones were classified in these images: percolation, slush and wet snow radar zone. Positive surface air temperatures and rainfall events, registered from a meteorological station, lead to increase in wet snow and slush zones. The COSMO-SkyMed images and minimum distance algorithm were adequate to discriminate the snow cover and to assess the supraglacial melting pattern during the ablation season in the study area.
机译:这项工作分析了位于南极洲国王乔治岛的克拉科夫冰场上的雪覆盖的时空变化。本研究中使用了COSMO-SKYMED的高空间分辨率图像。这些X波段图像垂直和水平共偏振,并且它们的强度数据被转换为幅度(DB)。基于雪地区的邻接关系知识,Cosmo-Skymed图像分类为最小距离算法和分类后。高度测量,斜坡,方面和太阳辐射图,以支持宇宙涉及图像中的反向散射图案的解释。在这些图像中分类了三个雷达区:渗透,纤溶和湿雪雷达区。从气象站注册的积极面积空气温度和降雨事件,导致湿雪和浸出区域增加。 COSMO-SCEMED图像和最小距离算法足以区分雪覆盖,并在研究区域的消融季节评估Supraglacial熔化模式。

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