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. By using the multi-source data of meteorology over recent decades, thisstudy discovered a summertime “hollow wet pool” in the troposphere with acenter of high water vapor over the Asian water tower (AWT) on the TibetanPlateau (TP), which is indicated by a vertical transport “window” in thetroposphere. The water vapor transport in the upper troposphere extends fromthe vertical transport window over the TP with significant connectionsamong the Arctic, Antarctic and TP regions, highlighting the effect of the TP'svertical transport window of water vapor in the troposphere on global changein water vapor. The vertical transport window is built by the AWT's thermalforcing in association with the dynamic effect of the TP's “hollow heatisland”. Our study improves the understanding of the vapor transport overthe TP with important implication for global climate change.

A vertical transport window of water vapor in the troposphere over the Tibetan Plateau with implications for global climate change