Warming, permafrost thaw and increased nitrogen availability as drivers for plant composition and growth across the Tibetan Plateau
Author:
Publisher
Elsevier BV
Subject
Soil Science,Microbiology
Reference40 articles.
1. Permafrost thaw and liberation of inorganic nitrogen in Eastern Siberia;Beermann;Permafrost and Periglacial Processes,2017
2. Delta progradation in Greenland driven by increasing glacial mass loss;Bendixen;Nature (London),2017
3. Plant functional trait change across a warming tundra biome;Bjorkman;Nature (London),2018
4. Dwelling in the deep-strongly increased root growth and rooting depth enhance plant interactions with thawing permafrost soil;Blume‐Werry;New Phytologist,2019
5. Assessment of past, present and future environmental changes on the Tibetan Plateau;Chen;Chinese Science Bulletin,2015
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1. Changes in above- versus belowground biomass distribution in permafrost regions in response to climate warming;Proceedings of the National Academy of Sciences;2024-06-10
2. Effects of nitrogen deposition with phosphorus addition on desert steppe plant communities;Agriculture, Ecosystems & Environment;2024-06
3. Research progress and perspectives on ecological processes and carbon feedback in permafrost wetlands under changing climate conditions;Fundamental Research;2024-05
4. Data-driven assessment of soil total nitrogen on the Qinghai-Tibet Plateau;Science of The Total Environment;2024-03
5. Warming and increasing precipitation induced greening on the northern Qinghai-Tibet Plateau;CATENA;2023-12
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