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Estimation of Minimum Land Surface Temperature Using MODIS LST Product for the Himalayan region

机译:Modis LST产品为喜马拉雅地区的MODIS LST产品估算最小土地表面温度

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Surface temperature distribution is a governing meteorological factor for studies investigating the hydrological and climatic behavior of a basin. In the Himalayan mountainous region, it is difficult to obtain the high resolution spatial records of the surface temperature because of the scarce and widely scattered meteorological stations. In this study, the potential of MODIS (Moderate Resolution Imaging Spectroradiometer) land surface temperature (LST) products such as MOD11A2 and MYD11A2 Collection 6 has been investigated for estimating accurate 8-Day minimum ground temperature (8DayMinT) values over Western Himalayan region. The forward, backward and stepwise variable selection methods have been employed for 8 major variables (including: LST products (four variables), altitude, latitude, longitude, and Julian day) and regression models have been formulated for 8DayMinT estimations. The results show that the regional topography explains most of the differences between the MODIS LST and the ground temperature records derived from the 7 climate stations in the Himalayan region. The best results for 8DayMinT estimation has been achieved when a combination of all the 4 LST products of TERRA and AQUA, along with altitude, latitude and longitude data is employed.
机译:表面温度分布是研究盆地水文和气候行为的研究的控制气象因素。在喜马拉雅山区,由于稀缺和广泛散射的气象站,难以获得表面温度的高分辨率空间记录。在该研究中,已经研究了MOD11A2和MYD11A2系列诸如MOD11A2和MYD11A2系列的诸如MOD11A2和MYD11A2收集6的潜在潜力,以估算HIMALAYAN地区的准确为8天的最小地温(80dint)值。已经采用了前进,倒退和逐步的变量选择方法(包括:LST产品(四个变量),高度,纬度,经度和朱利安日)和回归模型已为8daymint估计配制。结果表明,区域地形解释了MODIS LST与占Himalayan地区的7个气候站所源的大部分差异。当采用海拔,纬度和经度数据的所有4 LST产品的组合时,已经实现了8daymint估计的最佳结果。

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