摘要
<正>The climate effects of the Tibetan Plateau(TP) have been studied extensively in the past decades. However, most previous studies have focused merely on atmospheric processes. The interactions among multi-spheres(atmosphere, hydrosphere, biosphere, lithosphere, and anthroposphere) associated with the large-scale orography have received increasing interest recently[1,2], and particularly the air-sea interactions within the context of TP’s climatic impact have received progressive research attention in the last decade [3-8].
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