Due to insufficient palaeo-environmental records, the vegetation history and hydrology of the
Tibetan Plateau during the Last Glacial Maximum (LGM) are uncertain. In this study, a 316 …

Abstract Knowledge of paleotemperature variation in the Tibetan Plateau (TP) can provide
potential insights to evaluate the future climate change under ongoing global warming and …

Increasing extreme temperature, precipitation and rapid meltwater events have added stress
to the Himalaya's hydrological sensitivity and major flood risks, however, current extreme …

Natural archives of past larger floods provide insights for assessment of future extreme flood
events and climate variability in High Asian rivers. However, the sedimentary characteristics …

Stable isotopes are effective proxy indicators for past climate and environment changes.
Paleolimnological hydrogen and oxygen isotopes have been used to reconstruct changes in …

The scarcity of paleoclimate records in the western Tibetan Plateau (TP) hinders our
understanding of how environmental evolution affects past human population, agriculture …

Understanding the long‐term streamflow variability of the Yarlung Tsangpo (called the
Brahmaputra River in downstream) is critical for water resources management due to its …

Global warming has accelerated the degradation of permafrost and glaciers on the Tibetan
Plateau, resulting in a substantial release of meltwater that is affecting the regional …

The northern Chinese steppe is situated in the periphery of the East Asian Summer
Monsoon and exhibits high sensitivity to variations in monsoon intensity and global climate …