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dc.contributor.authorPiao, S
dc.contributor.authorNan, H
dc.contributor.authorHuntingford, C
dc.contributor.authorCiais, P
dc.contributor.authorFriedlingstein, P
dc.contributor.authorSitch, S
dc.contributor.authorPeng, S
dc.contributor.authorAhlström, A
dc.contributor.authorCanadell, JG
dc.contributor.authorCong, N
dc.contributor.authorLevis, S
dc.contributor.authorLevy, PE
dc.contributor.authorLiu, L
dc.contributor.authorLomas, MR
dc.contributor.authorMao, J
dc.contributor.authorMyneni, RB
dc.contributor.authorPeylin, P
dc.contributor.authorPoulter, B
dc.contributor.authorShi, X
dc.contributor.authorYin, G
dc.contributor.authorViovy, N
dc.contributor.authorWang, T
dc.contributor.authorWang, X
dc.contributor.authorZaehle, S
dc.contributor.authorZeng, N
dc.contributor.authorZeng, Z
dc.contributor.authorChen, A
dc.date.accessioned2016-02-04T11:55:48Z
dc.date.issued2014-10-16
dc.description.abstractSatellite-derived Normalized Difference Vegetation Index (NDVI), a proxy of vegetation productivity, is known to be correlated with temperature in northern ecosystems. This relationship, however, may change over time following alternations in other environmental factors. Here we show that above 30°N, the strength of the relationship between the interannual variability of growing season NDVI and temperature (partial correlation coefficient RNDVI-GT) declined substantially between 1982 and 2011. This decrease in RNDVI-GT is mainly observed in temperate and arctic ecosystems, and is also partly reproduced by process-based ecosystem model results. In the temperate ecosystem, the decrease in RNDVI-GT coincides with an increase in drought. In the arctic ecosystem, it may be related to a nonlinear response of photosynthesis to temperature, increase of hot extreme days and shrub expansion over grass-dominated tundra. Our results caution the use of results from interannual time scales to constrain the decadal response of plants to ongoing warming.en_GB
dc.description.sponsorshipStrategic Priority Research Program (B) of the Chinese Academy of Sciencesen_GB
dc.description.sponsorshipNational Basic Research Program of Chinaen_GB
dc.description.sponsorshipChinese Ministry of Environmental Protectionen_GB
dc.description.sponsorshipNational Natural Science Foundation of Chinaen_GB
dc.description.sponsorship111 Projecten_GB
dc.description.sponsorshipUS Department of Energy (DOE), Office of Science, Biological and Environmental Researchen_GB
dc.identifier.citationVol. 5, pp. 5018 -en_GB
dc.identifier.doi10.1038/ncomms6018
dc.identifier.grantnumberXDB03030404en_GB
dc.identifier.grantnumber2013CB956303en_GB
dc.identifier.grantnumber201209031en_GB
dc.identifier.grantnumber41125004en_GB
dc.identifier.grantnumber31321061en_GB
dc.identifier.grantnumberB14001en_GB
dc.identifier.grantnumberDE-AC05-00OR22725en_GB
dc.identifier.otherncomms6018
dc.identifier.urihttp://hdl.handle.net/10871/19597
dc.language.isoenen_GB
dc.publisherNature Publishing Groupen_GB
dc.relation.urlhttp://www.ncbi.nlm.nih.gov/pubmed/25318638en_GB
dc.relation.urlhttp://www.nature.com/ncomms/2014/141016/ncomms6018/full/ncomms6018.htmlen_GB
dc.rightsCopyright © 2014 Macmillan Publishers Limited. All Rights Reserved.en_GB
dc.subjectClimate scienceen_GB
dc.subjectBiogeochemistryen_GB
dc.subjectEarth sciencesen_GB
dc.titleEvidence for a weakening relationship between interannual temperature variability and northern vegetation activity.en_GB
dc.typeArticleen_GB
dc.date.available2016-02-04T11:55:48Z
exeter.place-of-publicationEngland
dc.descriptionJournal Articleen_GB
dc.descriptionResearch Support, Non-U.S. Gov'ten_GB
dc.descriptionResearch Support, U.S. Gov't, Non-P.H.S.en_GB
dc.identifier.eissn2041-1723
dc.identifier.journalNature Communicationsen_GB


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