Abstract The Third Pole (TP) is experiencing rapid warming and is currently in its warmest
period in the past 2,000 years. This paper reviews the latest development in multidisciplinary …

The stable oxygen isotope ratio (δ18O) in precipitation is an integrated tracer of atmospheric
processes worldwide. Since the 1990s, an intensive effort has been dedicated to studying …

Late Pleistocene sea level has been reconstructed from ocean sediment core data using a
wide variety of proxies and models. However, the accuracy of individual reconstructions is …

Prevailing opinion assigns the Tibetan Plateau a crucial role in sha** Asian climate,
primarily by heating of the atmosphere over Tibet during spring and summer. Accordingly …

Inter-annual variation in the ratio of 18 O to 16 O of precipitation (δ 18 O p) in the monsoon
regions of China (MRC, area approximately east of 100° E) has not yet been fully analyzed …

In this study, individual precipitation samples, collected over 2 years at stations in different
climatic regions of west China (Tibetan Plateau region, Tianshan region, and Altay) were …

Despite the importance of precipitation and moisture transport over the Tibetan Plateau for
glacier mass balance, river runoff and local ecology, changes in these quantities remain …

During the mid-1980s, there were 31 stations in China that successfully participated in the
Global Network of Isotopes in Precipitation. However, most observations were suspended …

Sedimentological data and hydrogen isotopic measurements of leaf wax long-chain n-
alkanes (δD wax) from an alpine lake sediment archive on the southeastern Tibetan Plateau …

In response to a request from Congress, Surface Temperature Reconstructions for the Last
2,000 Years assesses the state of scientific efforts to reconstruct surface temperature records …