Winter CH4 and CO2 Accumulation from a Permafrost Peatland Pond is Critical to Spring thaw Carbon Emissions
Author:
Funder
Fundamental Research Funds for the Central Universities
National Natural Science Foundation of China
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s13157-024-01852-1.pdf
Reference60 articles.
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2. Bégin PN, Tanabe Y, Rautio M, Wauthy M, Laurion I, Uchida M, Culley AI, Vincent WF (2021) Water column gradients beneath the summer ice of a high Arctic freshwater lake as indicators of sensitivity to climate change. Sci Rep 11(1):2868. https://doi.org/10.1038/s41598-021-82234-z
3. Boereboom T, Depoorter M, Coppens S, Tison JL (2012) Gas properties of winter lake ice in Northern Sweden: implication for carbon gas release. Biogeosciences 9(2):827–838. https://doi.org/10.5194/bg-9-827-2012
4. Burger M, Berger S, Spangenberg I, Blodau C (2016) Summer fluxes of methane and carbon dioxide from a pond and floating mat in a continental Canadian peatland. Biogeosciences 13:3777–3791. https://doi.org/10.5194/bg-13-3777-2016
5. Castro-Morales K, Kleinen T, Kaiser S, Zaehle S, Kittler F, Kwon MJ, Beer C, Göckede M (2018) Year-round simulated methane emissions from a permafrost ecosystem in Northeast Siberia. Biogeosciences 15(9):2691–2722. https://bg.copernicus.org/articles/15/2691/2018/
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