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Using Multi-Years MODIS LST Data to Monitor the Ground Surface Freezing and Thawing Conditions on the Qinghai-Tibet Plateau

机译:使用多年MODIS LST数据监控青藏高原上的地面冻结和解冻条件

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As the influence of global warming, it is important to assess the freezing and thawing conditions of the ground surface to fully understand the impacts of frozen ground on the surface and subsurface hydrology, the surface energy and moisture balance, ecosystem conservation, and engineering constructions on the Qinghai-Tibet Plateau (QTP). However, assessing the changes of ground surface freezing and thawing conditions on the QTP still remains a challenge owing to the sparseness and discontinuity of remote sensing and ground observations. The ground surface thawing index can be used to predict changes of the thermal regime of permafrost and can be good indicators of climate change in the QTP, which is of great importance for a variety of engineering applications. In this study, we firstly used the harmonic analysis of time series (HANTS) algorithm to fill in the Land Surface Temperatures (LST) data gaps of the Moderate Resolution Imaging Spectroradiometer (MODIS) observation data caused by the cloud contamination. Then we used the MODIS LST data to estimate the daily ground surface temperatures (GST) by a multiple linear regression model on the QTP. Finally, we calibrated the model by the ground temperature observations at a selection of meteorological stations. The precisely estimation of the multi-years thawing index within 2003-2012 is calculated to monitor the ground surface freezing and thawing conditions change on QTP.
机译:由于全球变暖的影响,评估地面的冻结和解冻条件是充分了解冻土对表面和地下水文的影响,表面能量和水分平衡,生态系统保护和工程结构的影响青藏高原(QTP)。然而,由于遥感和地面观测的稀释和不连续性,评估QTP上的地面冻结和解冻条件的变化仍然是一个挑战。地面解冻指数可用于预测永久冻土的热制度的变化,并且可以是QTP中气候变化的良好指标,这对于各种工程应用具有重要意义。在这项研究中,我们首先利用了时序序列(铰接)算法的谐波分析,填充了由云污染引起的中等分辨率成像光谱仪(MODIS)观测数据的陆地表面温度(LST)数据差距。然后我们使用MODIS LST数据通过QTP上的多个线性回归模型来估计日常地面温度(GST)。最后,我们通过在一系列气象站的地面温度观测中校准了模型。建议估计2003 - 2012年度的多年度解冻指数,以监测QTP对地面冻结和解冻条件的变化。

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