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dc.contributor.authorCarnicer, J
dc.contributor.authorDomingo-Marimon, C
dc.contributor.authorNinyerola, M
dc.contributor.authorCamarero, JJ
dc.contributor.authorBastos, A
dc.contributor.authorLópez-Parages, J
dc.contributor.authorBlanquer, L
dc.contributor.authorRodríguez-Fonseca, B
dc.contributor.authorLenton, TM
dc.contributor.authorDakos, V
dc.contributor.authorRibas, M
dc.contributor.authorGutiérrez, E
dc.contributor.authorPeñuelas, J
dc.contributor.authorPons, X
dc.date.accessioned2019-06-17T09:39:47Z
dc.date.issued2019-04-23
dc.description.abstractThe mechanisms translating global circulation changes into rapid abrupt shifts in forest carbon capture in semi-arid biomes remain poorly understood. Here we report unprecedented multidecadal shifts in forest carbon uptake in semi-arid Mediterranean pine forests in Spain over 1950-2012. The averaged carbon sink reduction varies between 31-37%, and reaches values in the range of 50% in the most affected forest stands. Regime shifts in forest carbon uptake are associated with climatic early warning signals, decreased forest regional synchrony, and reduced long-term carbon sink resilience. We identify the mechanisms linked to ocean multidecadal variability that shape regime shifts in carbon capture. Firstly, we show that low frequency variations of the surface temperature of the Atlantic Ocean induce shifts in the non-stationary effects of El Niño Southern Oscillation (ENSO) on regional forest carbon capture. Modelling evidence supports that the non-stationary effects of ENSO can be propagated from tropical areas to semi-arid Mediterranean biomes through atmospheric wave trains. Secondly, decadal changes of the Atlantic Multidecadal Oscillation (AMO) significantly alter sea-air heat exchanges, modifying in turn ocean vapour transport over land and land surface temperatures, and promoting sustained drought conditions in spring and summer that reduce forest carbon uptake. Thirdly, we show that lagged effects of AMO on the winter North Atlantic Oscillation (NAO) also contribute to the maintenance of long-term droughts. Finally, we show that the reported strong, negative effects of ocean surface temperature (AMO) on forest carbon uptake in the last decades are unprecedented over the last 150 years. Our results provide new, unreported explanations for carbon uptake shifts in these drought-prone forests and review the expected impacts of global warming on the profiled mechanisms. This article is protected by copyright. All rights reserved.en_GB
dc.description.sponsorshipNatural Environment Research Council (NERC)en_GB
dc.description.sponsorshipSpanish Government (MINECO/FEDER)en_GB
dc.description.sponsorshipConsolider Ingenio Montesen_GB
dc.description.sponsorshipEuropean Research Council Synergyen_GB
dc.description.sponsorshipEU H2020en_GB
dc.description.sponsorshipICREA Academia Excellenceen_GB
dc.identifier.citationPublished online 23 April 2019en_GB
dc.identifier.doi10.1111/gcb.14664
dc.identifier.grantnumberCGL2013-48074-Pen_GB
dc.identifier.grantnumberCGL013-48277-Pen_GB
dc.identifier.grantnumberCGL2010-17172en_GB
dc.identifier.grantnumberCGL2011-26654en_GB
dc.identifier.grantnumberCGL2012-33927en_GB
dc.identifier.grantnumberCGL2015-69888-Pen_GB
dc.identifier.grantnumberCGL2016-78093-Ren_GB
dc.identifier.grantnumberCSD2008-00040en_GB
dc.identifier.grantnumberAP2008-2016en_GB
dc.identifier.grantnumberCatalan Governmenten_GB
dc.identifier.grantnumberSGR2009-458en_GB
dc.identifier.grantnumberSGR2017-1690en_GB
dc.identifier.grantnumberSGR2017-1005en_GB
dc.identifier.grantnumberIMBALANCE-P (610028)en_GB
dc.identifier.grantnumberVENI-NWO 863.11.02en_GB
dc.identifier.grantnumberENV4-CT97-0641en_GB
dc.identifier.grantnumberECOPOTENTIAL (641762)en_GB
dc.identifier.grantnumber2016-2020 / 2011-2015en_GB
dc.identifier.urihttp://hdl.handle.net/10871/37548
dc.language.isoenen_GB
dc.publisherWIleyen_GB
dc.relation.urlhttps://www.ncbi.nlm.nih.gov/pubmed/31012512en_GB
dc.rights.embargoreasonUnder embargo until 23 April 2020 in compliance with publisher policy.en_GB
dc.rightsCopyright © 2019 John Wiley & Sons, Inc. All rights reserveden_GB
dc.titleRegime shifts of Mediterranean forest carbon uptake and reduced resilience driven by multidecadal ocean surface temperatures.en_GB
dc.typeArticleen_GB
dc.date.available2019-06-17T09:39:47Z
dc.identifier.issn1354-1013
exeter.place-of-publicationEnglanden_GB
dc.descriptionThis is the author accepted manuscript. The final version is available from Wiley via the DOI in this record.en_GB
dc.identifier.journalGlobal Change Biologyen_GB
dc.rights.urihttp://www.rioxx.net/licenses/all-rights-reserveden_GB
dcterms.dateAccepted2019-04-23
exeter.funder::Natural Environment Research Council (NERC)en_GB
rioxxterms.versionAMen_GB
rioxxterms.licenseref.startdate2019-04-23
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2019-06-17T09:22:42Z
refterms.versionFCDAM
refterms.panelCen_GB


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