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Snow cover and land surface temperature assessment of Gangotri basin in the Indian Himalayan Region (IHR) using MODIS satellite data for climate change inferences

机译:印度喜马拉雅地区甘蓝盆地的雪覆盖和陆地表面温度评估(IHR),使用Modis卫星数据进行气候变化推论

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Climate change has become a cause of concern as well as the challenge of this century. Himalayan mountain ranges with high snow fields and numerous valley glaciers may bear the brunt of such changes already being reported including Intergovernmental Panel on Climate Change (IPCC). Gangotri is one of the most prominent snow-fed catchments of Indian Himalayan Region (IHR) due to origin of river Ganga situated within it. Spatio-temporal changes in snow covered area of this basin were examined for melting seasons of the years 2006 to 2010 and a latest reference year of 2012 as a special test case. Standard snow data products (MOD10A2) of Moderate Resolution Imaging Spectroradiometer (MODIS)-Terra sensor with spatial resolution of 500 m were used. For all the years of reference, snow covered area percentage was derived for respective months representing usual ablation or melting periods. Snow depletion curves (SDCs) were generated for such periods of the respective years. CARTOSAT digital elevation model (DEM) was used for topographic information of terrain. Relationship of SDCs with the land surface temperatures (LST) of the basin was worked upon using MODIS-Terra LST (MOD11A2) product (version 5) with 1 km resolution at 8-day interval for the day time temperature for respective months of above reference years. Thereafter, interpolation and simulation of snow covered areas was carried out on the basis of LST data. The study thus produced snow cover maps for the years of reference as well as their relationship with LST for climate change inferences.
机译:气候变化已成为关注的原因以及本世纪的挑战。喜马拉雅山脉高雪场和众多山谷冰川的范围可能会承担已经报告的这些变化的冲突,包括政府间气候变化(IPCC)。由于江江河内的起源,甘蓝是印度喜马拉雅地区(IHR)最突出的雪地养殖集水区之一。在2006年至2010年融化的季节和2012年作为特殊考试案件的最新参考赛中,检查了这条盆地的雪覆盖区域的时空变化。使用500米的空间分辨率的适度分辨率成像光谱仪(MODIS) - 跨度传感器的标准雪数据产品(MOD10A2)。对于所有多年的参考日,达到雪覆盖的面积百分比,各个月份代表通常的消融或融化期。在各个年份的阶段产生雪消耗曲线(SDC)。 Cartosat数字高度模型(DEM)用于地形的地形信息。使用Modis-Terra LST(Mod11A2)产品(版本5)在盆地的陆地表面温度(Mod11A2)产品(5)分辨率为8天的时间温度以进行上述几个月的时间温度,工作年。此后,基于LST数据进行积雪区域的插值和仿真。因此,研究产生了多年的雪覆盖图以及与气候变化推论的LST的关系。

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