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Xiaoying Jin

Researcher at Chinese Academy of Sciences

Publications -  15
Citations -  579

Xiaoying Jin is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Permafrost & Soil water. The author has an hindex of 9, co-authored 15 publications receiving 226 citations. Previous affiliations of Xiaoying Jin include University of Alaska Fairbanks & Northeast Forestry University.

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Impacts of climate-induced permafrost degradation on vegetation: A review

TL;DR: In this paper, the impact of permafrost degradation on vegetation succession trajectories and associated changes in soil hydrology and soil nutrient above degrading permfrost was investigated in arctic and boreal regions.
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Thermal regime of warm-dry permafrost in relation to ground surface temperature in the Source Areas of the Yangtze and Yellow rivers on the Qinghai-Tibet Plateau, SW China

TL;DR: The thermal regime of warm-dry permafrost in the SAYYR was systematically analyzed based on extensive data collected during 2010-2016 of air temperature, ground surface temperature (GST) and ground temperature across a range of areas with contrasting land-surface characteristics and it is concluded that the accurate mapping ofpermafrost on the rugged elevational QTP could be potentially obtained by correlating the parameters of GST, thermal offset, and temperature gradient in the shallow permaf frost.
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Evolution of permafrost in China during the last 20 ka

TL;DR: In this article, the formation and evolution of permafrost in China during the last 20 ka were reconstructed on the basis of large amount of paleo-permafrost remains and paleo periglacial evidence, as well as paleoglacial landforms, paleoflora and paleofauna records.
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Delineating the hydrological processes and hydraulic connectivities under permafrost degradation on Northeastern Qinghai-Tibet Plateau, China

TL;DR: In this article, the authors used stable isotopic method and field hydrological observation to study the hydraulic connectivities between precipitation, stream water, thermokarst lakes, spring, and near-surface ground ice.