UVicSpace

Latitudinal limits to the predicted increase of the peatland carbon sink with warming

Show simple item record

dc.contributor.author Gallego-Sala, Angela V.
dc.contributor.author Charman, Dan J.
dc.contributor.author Brewer, Simon
dc.contributor.author Page, Susan E.
dc.contributor.author Prentice, I. Colin
dc.contributor.author Friedlingstein, Pierre
dc.contributor.author Moreton, Steve
dc.contributor.author Lacourse, Terri
dc.contributor.author et. al.
dc.date.accessioned 2019-01-17T18:00:13Z
dc.date.copyright 2018 en_US
dc.date.issued 2018
dc.identifier.citation Gallego-Sala, A.V., Charman, D.J., Brewer, S., Page, S.E., Prentice, I.C., Friedlingstein, P., … Zhao, Y. (2018). Latitudinal limits to the predicted increase of the peatland carbon sink with warming, Nature Climate Change, 8, 907-913. https://doi.org/10.1038/s41558-018-0271-1 en_US
dc.identifier.uri https://doi.org/10.1038/s41558-018-0271-1
dc.identifier.uri https://dspace.library.uvic.ca//handle/1828/10518
dc.description.abstract 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. en_US
dc.description.sponsorship The work presented in this paper was funded by the Natural Environment Research Council (NERC standard grant number NE/I012915/1) to D.J.C., A.G.S., I.C.P., S.P. and P.F., supported by NERC Radiocarbon Allocation 1681.1012. The work and ideas in this paper have also been supported by PAGES funding, as part of C-PEAT. C.D.J. was supported by the Joint UK DECC/Defra Met Office Hadley Centre Climate Programme (GA01101). This research is also a contribution to the AXA Chair Programme in Biosphere and Climate Impacts and the Imperial College initiative on Grand Challenges in Ecosystems and the Environment. This research was also supported by a grant from the National Science Centre, Poland 2015/17/B/ST10/01656. en_US
dc.language.iso en en_US
dc.publisher Nature Climate Change en_US
dc.subject peatlands en_US
dc.subject carbon cycle en_US
dc.subject climate change en_US
dc.subject tropical peat en_US
dc.subject last millennium en_US
dc.title Latitudinal limits to the predicted increase of the peatland carbon sink with warming en_US
dc.type Postprint en_US
dc.description.scholarlevel Faculty en_US
dc.description.reviewstatus Reviewed en_US
dc.description.embargo 2019-03-10


Files in this item

This item appears in the following Collection(s)

Show simple item record

Search UVicSpace


Browse

My Account

Statistics

Help