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Yafeng Shi
Researcher at Chinese Academy of Sciences
Publications - 13
Citations - 1414
Yafeng Shi is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Ice core & Plateau. The author has an hindex of 11, co-authored 13 publications receiving 1268 citations.
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Characteristics of late Quaternary monsoonal glaciation on the Tibetan Plateau and in East Asia
TL;DR: In this paper, it was shown that there was no Quaternary unified ice sheet developed in the Tibetan Plateau and that the change in equilibrium line depression was caused by the combined effect of the decrease in precipitation, the expansion of extreme continental glaciers and the active uplift of glaciated mountains.
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Reconstruction of the 30–40 ka bp enhanced Indian monsoon climate based on geological records from the Tibetan Plateau
TL;DR: In this article, multi-proxy records from ice caps, lakes and pollen records from the Tibetan Plateau are used to reconstruct the palaeoclimate during the period 30-40-ka bp.
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Estimation on the response of glaciers in China to the global warming in the 21st century
Yafeng Shi,Shiyin Liu +1 more
TL;DR: Wang et al. as mentioned in this paper classified the glaciers in China into three types: the maritime (temperate) type, sub-continental (sub-polar) type and extreme continental (polar), which take 22, 46% and 32% of the total existing glacier area.
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Climate variation since the Last Interglaciation recorded in the Guliya ice core
Tandong Yao,Lonnie G. Thompson,Lonnie G. Thompson,Yafeng Shi,Dahe Qin,Keqin Jiao,Zhihong Yang,Lide Tian,E. M. Thompson,E. M. Thompson +9 more
TL;DR: In this article, the authors reconstructed the climatic and environmental variations since the Last Interglaciation based on the study of the upper 268 m of the 309m-long Guliya ice core.
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Amplitude of climatic changes in Qinghai-Tibetan Plateau
TL;DR: In this paper, the authors focused on the problems related to the sensitivity of temporal and spatial changes of the climate in high-altitude regions, particularly in the Qinghai-Tibetan (Q-T) Plateau.