Negative feedback processes following drainage slow down permafrost degradation.

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第一作者： Mathias,Göckede

第一单位： Max Planck Institute for Biogeochemistry, Jena, Germany.

作者： Mathias,Göckede ^[1] ; Min Jung,Kwon ^[1] ; Fanny,Kittler ^[2] ; Martin,Heimann ^[1] ; Nikita,Zimov ^[1] ; Sergey,Zimov ^[3]

作者单位： Max Planck Institute for Biogeochemistry, Jena, Germany. ^[1] Korea Polar Research Institute, Incheon, South Korea. ^[2] Institute for Atmospheric and Earth System Research (INAR)/Physics, University of Helsinki, Helsinki, Finland. ^[3] North-East Scientific Station, Pacific Institute for Geography, Far-East Branch, Russian Academy of Sciences, Cherskii, Russia. ^[4] Far Eastern Federal University, Vladivostok, Russia. ^[5]

关键词 Arctic climate change drainage disturbance energy redistribution long-term effects permafrost carbon

主题词北极地区(Arctic Regions);气候变化(Climate Change);生态系统(Ecosystem);土壤(Soil)

DOI 10.1111/gcb.14744

PMID 31241797

发布时间 2023-10-19

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