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Lide Tian

Researcher at Chinese Academy of Sciences

Publications -  102
Citations -  5366

Lide Tian is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Precipitation & Monsoon. The author has an hindex of 33, co-authored 81 publications receiving 4235 citations. Previous affiliations of Lide Tian include Institute of Arctic and Alpine Research & Center for Excellence in Education.

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A review of climatic controls on δ18O in precipitation over the Tibetan Plateau: Observations and simulations

TL;DR: In this article, the authors established a database of precipitation δ18O and used different models to evaluate the climatic controls of precipitation over the Tibetan Plateau (TP), revealing three distinct domains associated with the influence of the westerlies (northern TP), Indian monsoon (southern TP), and transition in between.
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Stable isotopic variations in west China: A consideration of moisture sources

TL;DR: In this paper, the authors identify regional patterns in both δ18O and deuterium excess (D excess), defined as δD − 8δ 18O, and in particular the northward maximum extent of the southwest monsoon over the Tibetan Plateau.
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Tibetan Plateau summer monsoon northward extent revealed by measurements of water stable isotopes

TL;DR: In this article, a program of individual precipitation events and river water sampling and of water isotopic measurements (δD, δ18O) was carried out during summer 1996 along a northeast/southwest transect of the Tibetan Plateau.
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Oxygen-18 concentrations in recent precipitation and ice cores on the Tibetan Plateau

TL;DR: In this article, a detailed study of the climatic significance of δ18O in precipitation was completed on a 1500 km southwest-northeast transect of the Tibetan Plateau in central Asia.
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Response of inland lake dynamics over the Tibetan Plateau to climate change

TL;DR: Based on satellite images and extensive field investigations, Wang et al. as discussed by the authors demonstrate that a coherent lake growth on the Tibetan Plateau (TPI) has occurred since the late 1990s in response to a significant global climate change.