Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/29154
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dc.contributor.authorChapman, Daniel Sen_UK
dc.date.accessioned2019-03-30T01:02:50Z-
dc.date.available2019-03-30T01:02:50Z-
dc.date.issued2013-11en_UK
dc.identifier.urihttp://hdl.handle.net/1893/29154-
dc.description.abstractMountain plants are considered among the species most vulnerable to climate change, especially at high latitudes where there is little potential for poleward or uphill dispersal. Satellite monitoring can reveal spatiotemporal variation in vegetation activity, offering a largely unexploited potential for studying responses of montane ecosystems to temperature and predicting phenological shifts driven by climate change. Here, a novel remote-sensing phenology approach is developed that advances existing techniques by considering variation in vegetation activity across the whole year, rather than just focusing on event dates (e.g. start and end of season). Time series of two vegetation indices (VI), normalized difference VI (NDVI) and enhanced VI (EVI) were obtained from the moderate resolution imaging spectroradiometer MODIS satellite for 2786 Scottish mountain summits (600?1344 m elevation) in the years 2000?2011. NDVI and EVI time series were temporally interpolated to derive values on the first day of each month, for comparison with gridded monthly temperatures from the preceding period. These were regressed against temperature in the previous months, elevation and their interaction, showing significant variation in temperature sensitivity between months. Warm years were associated with high NDVI and EVI in spring and summer, whereas there was little effect of temperature in autumn and a negative effect in winter. Elevation was shown to mediate phenological change via a magnification of temperature responses on the highest mountains. Together, these predict that climate change will drive substantial changes in mountain summit phenology, especially by advancing spring growth at high elevations. The phenological plasticity underlying these temperature responses may allow long-lived alpine plants to acclimate to warmer temperatures. Conversely, longer growing seasons may facilitate colonization and competitive exclusion by species currently restricted to lower elevations. In either case, these results show previously unreported seasonal and elevational variation in the temperature sensitivity of mountain vegetation activity.en_UK
dc.language.isoenen_UK
dc.publisherJohn Wiley & Sons, Ltd (10.1111)en_UK
dc.relationChapman DS (2013) Greater phenological sensitivity to temperature on higher Scottish mountains: new insights from remote sensing. Global Change Biology, 19 (11), pp. 3463-3471. https://doi.org/10.1111/gcb.12254en_UK
dc.rightsThe publisher does not allow this work to be made publicly available in this Repository. Please use the Request a Copy feature at the foot of the Repository record to request a copy directly from the author. You can only request a copy if you wish to use this work for your own research or private study.en_UK
dc.rights.urihttp://www.rioxx.net/licenses/under-embargo-all-rights-reserveden_UK
dc.subjectalpine vegetationen_UK
dc.subjectclimate changeen_UK
dc.subjectecosystem phenologyen_UK
dc.subjectEVIen_UK
dc.subjectMODISen_UK
dc.subjectNDVIen_UK
dc.subjectsatellite monitoringen_UK
dc.titleGreater phenological sensitivity to temperature on higher Scottish mountains: new insights from remote sensingen_UK
dc.typeJournal Articleen_UK
dc.rights.embargodate2999-12-31en_UK
dc.rights.embargoreason[Chapman-2013-Global_Change_Biology.pdf] The publisher does not allow this work to be made publicly available in this Repository therefore there is an embargo on the full text of the work.en_UK
dc.identifier.doi10.1111/gcb.12254en_UK
dc.identifier.pmid23661383en_UK
dc.citation.jtitleGlobal Change Biologyen_UK
dc.citation.issn1365-2486en_UK
dc.citation.issn1354-1013en_UK
dc.citation.volume19en_UK
dc.citation.issue11en_UK
dc.citation.spage3463en_UK
dc.citation.epage3471en_UK
dc.citation.publicationstatusPublisheden_UK
dc.citation.peerreviewedRefereeden_UK
dc.type.statusVoR - Version of Recorden_UK
dc.contributor.funderNatural Environment Research Councilen_UK
dc.author.emaildaniel.chapman@stir.ac.uken_UK
dc.citation.date09/05/2013en_UK
dc.contributor.affiliationCentre for Ecology & Hydrologyen_UK
dc.identifier.isiWOS:000325567100019en_UK
dc.identifier.scopusid2-s2.0-84885429137en_UK
dc.identifier.wtid1100321en_UK
dc.contributor.orcid0000-0003-1836-4112en_UK
dc.date.accepted2013-04-30en_UK
dcterms.dateAccepted2013-04-30en_UK
dc.date.filedepositdate2019-03-07en_UK
rioxxterms.apcnot requireden_UK
rioxxterms.typeJournal Article/Reviewen_UK
rioxxterms.versionVoRen_UK
local.rioxx.authorChapman, Daniel S|0000-0003-1836-4112en_UK
local.rioxx.projectProject ID unknown|Natural Environment Research Council|http://dx.doi.org/10.13039/501100000270en_UK
local.rioxx.freetoreaddate2263-04-10en_UK
local.rioxx.licencehttp://www.rioxx.net/licenses/under-embargo-all-rights-reserved||en_UK
local.rioxx.filenameChapman-2013-Global_Change_Biology.pdfen_UK
local.rioxx.filecount1en_UK
local.rioxx.source1365-2486en_UK
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