There is much debate regarding the temporal and spatial pattern of hydroclimate variations
on the Tibetan Plateau during the Holocene, focusing especially on the dipolar pattern of …

The pattern of changes in Holocene moisture conditions in the southern Tibetan Plateau
(TP) and the associated driving mechanism are still controversial. Here, we present the …

Quantifying the timing and extent of Quaternary mountain glaciations can help us in
understanding the cause of ice-age cycles. As such, impressive achievements have been …

Reconstructing vegetation and climate changes after the Last Glacial Maximum on the
Tibetan Plateau (TP) is a key to understand past Indian Summer Monsoon (ISM) dynamics …

Abstract The Serling Co region is located at the transitional zone of the interaction between
the Indian monsoon and the westerlies over the Tibetan Plateau. The Serling Co lake covers …

青藏高原气候变化在冰期-间冰期, 千年, 十年际和季节尺度上受亚洲季风和西风环流的交互影响,
表现出显著的区域性特征. 然而全新世以来青藏高原气候变化的机制还不甚清楚 …

Lake-level reconstructions aid in clarifying the relationship between climatic and
hydrological changes and serve as a reference for predicting future hydrological evolution …

Mountain glaciers are sensitive to climate change, and can provide valuable information for
inferring former climates on the Tibetan Plateau (TP). The increasing glacial chronologies …

Climate change characteristics in the Qinghai-Tibetan Plateau (QTP) exhibit spatial
differences. These differences are due to different large circulation systems, comprising …

Our knowledge of the influence of the Westerlies on the hydroclimate of High Mountain Asia
during the Holocene, especially during the mid-Holocene, remains poorly understood …