Climate change on the Tibetan Plateau (TP) and its response to the atmosphere circulation
has been widely concerned. The extremely cold-dry area of the central-northern TP is …

As a transitional zone between westerlies and the Asian Monsoon system, the northeastern
part of the Tibetan Plateau (NETP) is highly sensitive to climate change. The record of …

To understand the vegetation succession and climatic changes at the southeastern margin
of the Tibetan Plateau in the Neogene, we reconstructed the Middle Miocene vegetation and …

The climate conditions during the Little Ice Age (LIA) provide immediate background for
assessing current climate warming. In this paper, the spatial and temporal climate variability …

Abstract The northern Tibetan Plateau is a climatically sensitive zone influenced by
monsoon and westerly winds. In summer, water vapor transport can reach Qinghai Lake and …

Pollen evidence from sediment cores at Hurleg and Toson lakes in the Qaidam Basin was
obtained to examine vegetation and climatic change in the northeastern Qinghai-Tibetan …

Peat sediments and peatland evolution process offer abundant clues into the history of
vegetation and climate changes. In order to reconstruct Holocene peatland, vegetation and …

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 …

Based on the monthly precipitation and evaporation data from 139 meteorological stations in
the southeast side of the Tibetan Plateau and NCEP reanalysis data with 2.5× 2.5 spatial …

ABSTRACT Spatial and temporal variations in moisture across the Tibetan Plateau (TP)
during the years 1300-2005 were investigated using 50 gridded Palmer drought severity …