随着全球气候变化研究的深入，青藏高原加热的区域和全球气候效应越来越受到关注。关于青藏高原加热的时空特征，其对东亚、南亚天气气候的影响，已经取得了丰硕的成果；而对南亚高压西侧的欧洲、非洲中低纬大气环流研究甚少。并且南亚高压南侧的印度洋高低层大气环流配置又与非洲大气环流和青藏高原加热都有密切联系。因此，本项目将利用台站观测资料、卫星资料和再分析资料系统分析青藏-伊朗高原表面-大气加热的时空特征和联系；研究其加热对南亚高压西部（强度和范围等），热带东风急流，非洲季风，印度洋上空的transverse环流等欧洲-非洲-印度洋（欧-非-印）中低纬大气环流和季风系统的影响和内在物理机制；并分析青藏-伊朗高原加热对全球关键区海温与欧-非-印中低纬大气环流和季风系统的关系的调制作用。

With the deepening of global climate change research, the regional and global climate effects of the heating over the Tibetan Plateau have been paid more and more attention. The researches on the spatial and temporal characteristics of the Tibetan heating and its impact on the weather and climate over East Asia and South Asia have achieved fruitful results. However, little research has been done on the mid-lower latitude Europe-Africa atmospheric circulations on the west of South Asia high. In addition, the high and low level atmospheric circulation configuration over the India Ocean is closely related to both the African atmospheric circulation and the heating over the Tibetan Plateau. Therefore, the proposal will analyze the temporal and spatial characteristics of the atmospheric and surface heating over the Tibetan Plateau and the Iran Plateau and their relation between them, examine the heating influence on Europe-Africa-Indian Ocean atmospheric circulations at the mid-lower latitudes such as the west of South Asia high (intensity and range), the tropical easterly jet, the African monsoon, the transverse circulation over the Indian Ocean, and the intrinsic physical mechanism among them, and study the modulation effect of heating over the Tibetan Plateau and the Iranian Plateau for the relationship between SSTs in the global critical areas and Europe-Africa-Indian Ocean atmospheric circulations and monsoon systems at the mid-lower latitudes, by using the station observation data, satellite data and reanalysis data.