Abstract The Tibetan Plateau (TP) impacts local and remote atmospheric circulations,
wherein it mechanically and thermally affects air masses or airflows. Moreover, the TP …

Global-scale glacier shrinkage is one of the most prominent signs of ongoing climatic
change. However, important differences in glacier response exist at the regional scale, and …

Reliable precipitation data are highly necessary for geoscience research in the Third Pole
(TP) region but still lacking, due to the complex terrain and high spatial variability of …

Abstract The High Asia Refined analysis (HAR) is a regional atmospheric data set generated
by dynamical downscaling of the Final operational global analysis (FNL) using the Weather …

Volume changes and water balances of the lakes on the Tibetan Plateau (TP) are spatially
heterogeneous and the lake-basin scale drivers remain unclear. In this study, we …

Evidence has suggested a wetting trend over part of the Tibetan Plateau (TP) in recent
decades, although there are large uncertainties in this trend due to sparse observations …

High-accuracy meteorological datasets are urgently required for understanding hydrological
processes across the Third Pole (Qinghai-Tibetan Plateau, or TP), where meteorological …

There remains substantial debate concerning the relative roles of tectonics and of global
climate in pacing the evolution of aridity in Central Asia over the Cenozoic. Tibetan Plateau …

Current climate models commonly overestimate precipitation over the Tibetan Plateau (TP),
which limits our understanding of past and future water balance in the region. Identifying …

Long-range transport of black carbon from South Asia to the Tibetan plateau and its
deposition on glaciers directly enhances glacier melt. Here we find South Asian black …