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Extraction of Snow Cover Fraction and Snow Depth in South Korea from MODIS images

机译:从MODIS影像中提取韩国积雪覆盖率和积雪深度

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Observations in the visible and infrared spectral bands from the MODerate resolution Imaging Spectroradiometer (MODIS) have been used to derive snow depth from snow albedo. The information on the snow depth has been widely used in hydrological and numerical weather prediction, disaster managements and other environmental applications. Among the remote-sensed imaging systems, the Terra/Aqua MODIS satellite imaging systems have demonstrated success in surface monitoring, because they have been acquired for over ten years with 98-99 minutes repeat cycle. In this study, we create snow depth maps for three heavy snowfall events in South Korea, which occurred in January 2010, February 2011 and December 2012. In order to estimate the snow depths from satellite images, the following three steps are needed: 1) the generation of a snow cover map from the Normalized Difference Snow Index (NDSI), 2) the creation of the snow fraction cover map from the generated snow cover map, and 3) the production of the snow depth map from the snow fraction cover map. In order to establish a statistical relationship between satellite-observed snow fraction and snow depth, we have used snow depth data over the South Korea reported from NCDSS (National Climate Data Service System) stations. For the validation of the results, we compare the snow depths estimated from MODIS images with the in-situ observations.
机译:MODerate分辨率成像光谱仪(MODIS)在可见和红外光谱带中的观测已被用于从雪反照率中推算出雪深。关于积雪深度的信息已广泛用于水文和数值天气预报,灾害管理和其他环境应用中。在遥感成像系统中,Terra / Aqua MODIS卫星成像系统已在表面监测方面取得了成功,因为它们已经以十年的周期(98-99分钟的重复周期)获得了成功。在这项研究中,我们为2010年1月,2011年2月和2012年12月发生的韩国的三场大雪事件创建了雪深图。为了从卫星图像估算雪深,需要执行以下三个步骤:1)根据规范化差异雪指数(NDSI)生成积雪图,2)根据生成的积雪图创建积雪图,3)根据积雪图生成积雪深度图。为了建立卫星观测的降雪分数与降雪深度之间的统计关系,我们使用了NCDSS(国家气候数据服务系统)站报告的韩国降雪深度数据。为了验证结果,我们将MODIS影像估计的积雪深度与现场观测结果进行了比较。

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