Abstract Groundwater 18O/16O, 2H/1H, 13C/12C, 3H, and 14C data can help quantify
molecular movements and chemical reactions governing groundwater recharge, quality …

Abstract Climate changes on Southeastern Tibetan Plateau have important impacts on
social and economic development, as well as the ecosystem of southwestern China and …

Precipitation stable isotope is a good medium for studying the water cycle and atmospheric
water vapor transport process. To better understand the influence and control mechanism of …

The strong present-day Asian monsoons are thought to have originated between 25 and 22
million years (Myr) ago, driven by Tibetan–Himalayan uplift. However, the existence of older …

Global climate change varies greatly in different regions, so it is necessary to
comprehensively analyze climate change in different regions through different indicators …

Carbonate cave deposits in India and China are assumed to record the intensity of monsoon
precipitation, because the δ18O of the carbonate tracks the isotopic signature of …

Qunf Cave oxygen isotope (δ18Oc) record from southern Oman is one of the most significant
of few Holocene Indian summer monsoon cave records. However, the interpretation of the …

Indian Summer Monsoon (ISM) precipitation during the twentieth century is characterized by
a biennial oscillation, such that ISM precipitation varied between singularly strong and weak …

Speleothem proxy records from northeastern (NE) India reflect seasonal changes in Indian
summer monsoon strength as well as moisture source and transport paths. We have …

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 …