Decadal increases in carbon uptake offset by respiratory losses across northern permafrost ecosystems
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2024
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Details
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Journal Title:Nature Climate Change
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Personal Author:See, Craig R.
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Virkkala, Anna-Maria
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Natali, Susan M.
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Rogers, Brendan M.
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Mauritz, Marguerite
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Biasi, Christina
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Bokhorst, Stef
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Boike, Julia
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Bret-Harte, M. Syndonia
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Celis, Gerardo
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Chae, Namyi
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Christensen, Torben R.
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Murner, Sara June
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Dengel, Sigrid
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Dolman, Han
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Edgar, Colin W.
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Elberling, Bo
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Emmerton, Craig A.
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Euskirchen, Eugénie S.
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Göckede, Mathias
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Grelle, Achim
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Heffernan, Liam
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Helbig, Manuel
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Holl, David
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Humphreys, Elyn
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Iwata, Hiroki
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Järveoja, Järvi
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Kobayashi, Hideki
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Kochendorfer, John
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Kolari, Pasi
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Kotani, Ayumi
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Kutzbach, Lars
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Kwon, Min Jung
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Lathrop, Emma R.
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López-Blanco, Efrén
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Mammarella, Ivan
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Marushchak, Maija E.
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Mastepanov, Mikhail
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Matsuura, Yojiro
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Merbold, Lutz
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Meyer, Gesa
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Minions, Christina
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Nilsson, Mats B.
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Nojeim, Julia
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Oberbauer, Steven F.
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Olefeldt, David
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Park, Sang-Jong
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Parmentier, Frans-Jan W.
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Peichl, Matthias
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Peter, Darcy
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Petrov, Roman
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Poyatos, Rafael
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Prokushkin, Anatoly S.
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Quinton, William
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Rodenhizer, Heidi
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Sachs, Torsten
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Savage, Kathleen
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Schulze, Christopher
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Sjögersten, Sofie
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Sonnentag, Oliver
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St. Louis, Vincent L.
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Torn, Margaret S.
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Tuittila, Eeva-Stiina
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Ueyama, Masahito
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Varlagin, Andrej
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Voigt, Carolina
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Watts, Jennifer D.
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Zona, Donatella
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Zyryanov, Viacheslav I.
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Schuur, Edward A. G.
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NOAA Program & Office:
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Description:Tundra and boreal ecosystems encompass the northern circumpolar permafrost region and are experiencing rapid environmental change with important implications for the global carbon (C) budget. We analysed multi-decadal time series containing 302 annual estimates of carbon dioxide (CO2) flux across 70 permafrost and non-permafrost ecosystems, and 672 estimates of summer CO2 flux across 181 ecosystems. We find an increase in the annual CO2 sink across non-permafrost ecosystems but not permafrost ecosystems, despite similar increases in summer uptake. Thus, recent non-growing-season CO2 losses have substantially impacted the CO2 balance of permafrost ecosystems. Furthermore, analysis of interannual variability reveals warmer summers amplify the C cycle (increase productivity and respiration) at putatively nitrogen-limited sites and at sites less reliant on summer precipitation for water use. Our findings suggest that water and nutrient availability will be important predictors of the C-cycle response of these ecosystems to future warming.
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Source:Nature Climate Change, 14(8), 853-862
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DOI:
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ISSN:1758-678X ; 1758-6798
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Format:
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License:
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Rights Information:CC BY
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Compliance:Library
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Main Document Checksum:urn:sha-512:4bdae83b0a6f8437fdbc0df7f7921d6aee1e91d5413e40e2688ae0b0bc310d59a53c18de36d5f6288834c4ebe7ec0a117f1905d494b626d4e78437d33b185357
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