Long-term variation in surface heat and water exchange in the Tibetan Plateau and its effects on temperature increases

在这项研究中，我们对近几十年来由于大气温度升高而引起的青藏高原热收支和水收支变化进行了定量评价。首先，考虑局地观测环境变化的影响，对气象台气候资料进行重新评价。结果，我们得到了青藏高原上空大气温度的实际升高。接下来，我们开发了一种新的方法来评估地球表面的热量和水收支，包括湖泊和沼泽以及土壤和积雪。最后，利用卫星资料、再分析资料和气象台资料，对青藏高原的热收支和水收支进行了评估，并阐明了大气温度升高引起的长期变化趋势

In this study, we present a quantitative evaluation of the changes in the heat and water budgets of the Tibetan Plateau induced by the increase in atmospheric temperature over the last several decades. First, climate data obtained from meteorological observatories was re-evaluated by considering the influence of changes in the local observed environment. As a result, we obtained the actual increase in atmospheric temperature over the Tibetan Plateau. Next, we developed a new method for evaluating the heat and water budgets of the earth’s surface, including lakes and marshes as well as soil and snow cover. Finally, using satellite data and the reanalysis and meteorological observatory data, we evaluated the heat and water budgets of the Plateau and elucidated trends in their long-term changes induced by the increase in atmospheric temperature