Latitudinal limits to the predicted increase of the peatland carbon sink with warming
Autor: | Nicole K. Sanderson, Maara S. Packalen, Eric S. Klein, Robert K. Booth, Esther Githumbi, Joan Bunbury, Svante Björck, Julie Loisel, Katarzyna Marcisz, Donna Carless, I. Colin Prentice, Christopher Bochicchio, Colin J Courtney-Mustaphi, Jonathan E. Nichols, Rodney A. Chimner, John Hribjlan, Joana Zaragoza-Castells, Michael J. Clifford, Joanna Uglow, Patrick Moss, D. Mauquoy, James R. Holmquist, Charly Massa, Markku Mäkilä, Michelle Garneau, T. Edward Turner, David Large, Tim Mighall, Rob Marchant, Fraser J.G. Mitchell, Mariusz Lamentowicz, Sarah A. Finkelstein, Paul Mathijssen, Zicheng Yu, Antonio Martínez Cortizas, François De Vleeschouwer, Lisa C. Orme, Steve Moreton, Rixt de Jong, Chris D. Jones, Edgar Karofeld, A. Britta K. Sannel, Pirita Oksanen, Atte Korhola, Gaël Le Roux, Graeme T. Swindles, Ulla Kokfelt, Matthew J. Amesbury, Philip Camill, Thomas P. Roland, Helen Mackay, Tatiana Blyakharchuk, Susan Page, Gabriel Magnan, Glen M. MacDonald, Simon Brewer, Barbara Fiałkiewicz-Kozieł, Terri Lacourse, Noemí Silva-Sánchez, Paul D.M. Hughes, Stephen Robinson, Natascha Steinberg, Miriam C. Jones, Dan J. Charman, Angela V. Gallego-Sala, Martin Lavoie, Marjolein van der Linden, Elizabeth L. Cressey, Simon van Bellen, Guoping Wang, Yan Zhao, David W. Beilman, Bas van Geel, Pierre Friedlingstein, Minna Väliranta |
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Přispěvatelé: | Centre National de la Recherche Scientifique - CNRS (FRANCE), Institut National Polytechnique de Toulouse - INPT (FRANCE), Université Toulouse III - Paul Sabatier - UT3 (FRANCE), Institut National Polytechnique de Toulouse - Toulouse INP (FRANCE), University of Bristol [Bristol], University of Utah, Department of Geography [Leicester], University of Leicester, Macquarie University, Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Lund University [Lund], Centre National de la Recherche Scientifique (CNRS), University of Toronto, Université du Québec à Montréal = University of Québec in Montréal (UQAM), York Institute for Tropical Ecosystems, Environment Department, Wentworth Way, University of York [York, UK], University of Tartu, Geological Survey of Denmark and Greenland (GEUS), University of Helsinki, Department of Geography, University of Victoria [Canada] (UVIC), Argiles, Géochimie et Environnements sédimentaires - AGES (Liège, Belgium) (AGEs), Université de Liège, Uniwersytet im. Adama Mickiewicza w Poznaniu, Department of Chemical and Environmental Engineering, University of Nottingham, University of Nottingham, UK (UON), Université Laval [Québec] (ULaval), Lehigh University [Bethlehem], GEOTOP Research Center, Universite du Quebec a Montreal, Montreal, QC, Canada, Laboratoire Chrono-environnement - CNRS - UBFC (UMR 6249) (LCE), Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC), Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC), University of Aberdeen, Universidade de Santiago de Compostela [Spain] (USC ), University of New South Wales [Canberra Campus] (UNSW), BIAX Consult (NETHERLANDS), Vrije universiteit = Free university of Amsterdam [Amsterdam] (VU), Key Laboratory of Machine Perception (MOE), Peking University [Beijing], School of Geosciences [Edinburgh], University of Edinburgh, VU University Amsterdam, Natural Environment Research Council (NERC), AXA Research Fund, Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Helsingin yliopisto = Helsingfors universitet = University of Helsinki, Laboratoire Chrono-environnement (UMR 6249) (LCE), Vrije Universiteit Amsterdam [Amsterdam] (VU), Ecosystem and Landscape Dynamics (IBED, FNWI) |
Jazyk: | angličtina |
Rok vydání: | 2018 |
Předmět: |
Peat
010504 meteorology & atmospheric sciences Peatland [SDE.MCG]Environmental Sciences/Global Changes Climate change Growing season 010501 environmental sciences Environmental Science (miscellaneous) Atmospheric sciences 01 natural sciences Sink (geography) Carbon cycle Tropical peat Geosciences Multidisciplinary ComputingMilieux_MISCELLANEOUS 0105 earth and related environmental sciences Ecologie Environnement geography geography.geographical_feature_category Biogeochemistry Carbon sink 15. Life on land Multidisciplinär geovetenskap 13. Climate action [SDE]Environmental Sciences Environmental science Social Sciences (miscellaneous) |
Zdroj: | Nature Climate Change Nature Climate Change, Nature Publishing Group, 2018, 8 (10), pp.907-913. ⟨10.1038/s41558-018-0271-1⟩ Nature Climate Change, 2018, 8 (10), pp.907-913. ⟨10.1038/s41558-018-0271-1⟩ Nature Climate Change, 8(10), 907-913. Nature Publishing Group |
ISSN: | 1758-678X 1758-6798 |
DOI: | 10.1038/s41558-018-0271-1⟩ |
Popis: | The carbon sink potential of peatlands depends on the balance of carbon uptake by plants and microbial decomposition. The rates of both these processes will increase with warming but it remains unclear which will dominate the global peatland response. Here we examine the global relationship between peatland carbon accumulation rates during the last millennium and planetary-scale climate space. A positive relationship is found between carbon accumulation and cumulative photosynthetically active radiation during the growing season for mid- to high-latitude peatlands in both hemispheres. However, this relationship reverses at lower latitudes, suggesting that carbon accumulation is lower under the warmest climate regimes. Projections under Representative Concentration Pathway (RCP)2.6 and RCP8.5 scenarios indicate that the present-day global sink will increase slightly until around AD 2100 but decline thereafter. Peatlands will remain a carbon sink in the future, but their response to warming switches from a negative to a positive climate feedback (decreased carbon sink with warming) at the end of the twenty-first century. |
Databáze: | OpenAIRE |
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