Numerous studies of changes in the climate, vegetation and landscape responses of the
Tibetan Plateau (TP) during the Holocene have been published in recent decades …

Abstract Over the Tibetan Plateau (TP), lakes as paleoenvironmental archives have been
the most extensively investigated for their sensitivities to climate change on different …

The Tibetan Plateau is the highest and one of the most demanding environments ever
inhabited by humans. We investigated the timing and mechanisms of its initial colonization …

Lakes and vegetation are important factors of the Earth's hydrological cycle and can be
called an “indicator” of climate change. In this study, long-term changes of lakes' area and …

Qinghai Lake is of significance for paleoclimate research because it lies in a pivotal region
that is influenced by both the mid‐latitude Westerlies and the low‐latitude Asian summer …

Snow over the Tibetan Plateau (TP) is an important water source of major Asian rivers and
greatly influences water availability in the downstream areas. In this study, snow cover …

Lake high-stand sediments are found in three onshore terraces at Lake Donggi Cona,
northeastern Tibetan Plateau, and reveal characteristics of hydrological changes on lake …

Lake basins record critical interactions between the hydrosphere, cryosphere and
atmosphere. Their sediments and shoreline landforms archive timing, duration, and intensity …

Expansion or shrinkage of closed lakes is a natural response to fluctuations in precipitation
and evaporation, linked closely to changes in strength or position of atmospheric circulation …

Abstract Lakes in the Tibetan Plateau (TP) provide indications of the past global climate
change over this vast elevated highland. However, the patterns of Holocene lake-level …