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dc.creatorRodríguez Galiano, Víctor Franciscoes
dc.creatorDash, Jadunandanes
dc.creatorAtkinson, Peteres
dc.date.accessioned2018-05-08T09:22:28Z
dc.date.available2018-05-08T09:22:28Z
dc.date.issued2015
dc.identifier.citationRodríguez Galiano, V.F., Dash, J. y Atkinson, P. (2015). Characterising the Land Surface Phenology of Europe Using Decadal MERIS Data. Remore Sens, 7, 9390-9409.
dc.identifier.issn2072-4292es
dc.identifier.urihttps://hdl.handle.net/11441/74244
dc.description.abstractLand surface phenology (LSP), the study of the timing of recurring cycles of changes in the land surface using time-series of satellite sensor-derived vegetation indices, is a valuable tool for monitoring vegetation at global and continental scales. Characterisation of LSP and its spatial variation is required to reveal and predict ongoing changes in Earth system dynamics. This study presents and analyses the LSP of the pan-European continent for the last decade, considering three phenological metrics: onset of greenness (OG), end of senescence (EOS), and length of season (LS). The whole time-series of Multi-temporal Medium Resolution Imaging Spectrometer (MERIS) Terrestrial Chlorophyll Index (MTCI) data at 1 km spatial resolution was used to estimate the phenological metrics. Results show a progressive pattern in phenophases from low to high latitudes. OG dates are distributed widely from the end of December to the end of May. EOS dates range from the end of May to the end of January and the spatial distribution is generally the inverse of that of the OG. Shorter growing seasons (approximately three months) are associated with rainfed croplands in Western Europe, and forests in boreal and mountainous areas. Maximum LS values appear in the Atlantic basin associated with grasslands. The LSP maps presented in this study are supported by the findings of a previous study where OG and EOS estimates were compared to those of the pan-European phenological network at certain locations corresponding to numerous observations of deciduous tree plant species. Moreover, the spatio-temporal pattern of the OG and EOS produced close agreement with the dates of deciduous tree leaf unfolding and autumnal colouring, respectively (pseudo R-squared equal to 0.70 and 0.71 and root mean square error of six days (over 365 days)).es
dc.formatapplication/pdfes
dc.language.isoenges
dc.publisherMDPIes
dc.relation.ispartofRemore Sens, 7, 9390-9409.
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectLand surface phenologyes
dc.subjectMTCIes
dc.subjectBiogeographical regionses
dc.subjectLand coverses
dc.subjectSpringes
dc.subjectAutumnes
dc.titleCharacterising the Land Surface Phenology of Europe Using Decadal MERIS Dataes
dc.typeinfo:eu-repo/semantics/articlees
dcterms.identifierhttps://ror.org/03yxnpp24
dc.type.versioninfo:eu-repo/semantics/publishedVersiones
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
dc.contributor.affiliationUniversidad de Sevilla. Departamento de Geografía Física y Análisis Geográfico Regionales
dc.relation.publisherversionhttp://www.mdpi.com/2072-4292/7/7/9390es
dc.identifier.doi10.3390/rs70709390es
idus.format.extent20 p.es
dc.journaltitleRemore Senses
dc.publication.issue7es
dc.publication.initialPage9390es
dc.publication.endPage9409es
dc.identifier.sisius20848354es

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