Publication:
Temperature response to changes in vegetation fraction cover in a regional climate model

dc.contributor.authorJiménez Gutiérrez, José Manuel
dc.contributor.authorValero Rodríguez, Francisco
dc.contributor.authorRuiz Martínez, Jesús
dc.contributor.authorMontávez, Juan Pedro
dc.date.accessioned2023-06-17T09:13:58Z
dc.date.available2023-06-17T09:13:58Z
dc.date.issued2021-05-05
dc.description© 2021 by the authors. We acknowledge all the institutions and communities that provided free software, R community, CDO (Climate Data Operators), GMT (Generic Mapping Tools), MM5, Gnuplot,gfortran as well as the institutions supplying data (ECMWF, NASA).This study was supported by the Spanish Ministry of the Economy and Competitiveness/Agencia Estatal de Investigaciónand the European Regional Development Fund (ERDF/FEDER) through project ACEX-CGL2017-87921-R project.
dc.description.abstractVegetation plays a key role in partitioning energy at the surface. Meteorological and Climate Models, both global and regional, implement vegetation using two parameters, the vegetation fraction and the leaf area index, obtained from satellite data. In most cases, models use average values for a given period. However, the vegetation is subject to strong inter-annual variability. In this work, the sensitivity of the near surface air temperature to changes in the vegetation is analyzed using a regional climate model (RCM) over the Iberian Peninsula. The experiments have been designed in a way that facilitates the physical interpretation of the results. Results show that the temperature sensitivity to vegetation depends on the time of year and the time of day. Minimum temperatures are always lower when vegetation is increased; this is due to the lower availability of heat in the ground due to the reduction of thermal conductivity. Regarding maximum temperatures, the role of increasing vegetation depends on the available moisture in the soil. In the case of hydric stress, the maximum temperatures increase, and otherwise decrease. In general, increasing vegetation will lead to a higher daily temperature range, since the decrease in minimum temperature is always greater than the decrease for maximum temperature. These results show the importance of having a good estimate of the vegetation parameters as well as the implications that vegetation changes due to natural or anthropogenic causes might have in regional climate for present and climate change projections.
dc.description.departmentDepto. de Física de la Tierra y Astrofísica
dc.description.facultyFac. de Ciencias Físicas
dc.description.refereedTRUE
dc.description.sponsorshipMinisterio de Economía y Competitividad (MINECO)/FEDER
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/67894
dc.identifier.doi10.3390/atmos12050599
dc.identifier.issn2073-4433
dc.identifier.officialurlhttp://dx.doi.org/10.3390/atmos12050599
dc.identifier.relatedurlhttps://www.mdpi.com/2073-4433/12/5/599
dc.identifier.urihttps://hdl.handle.net/20.500.14352/8442
dc.issue.number5
dc.journal.titleAtmosphere
dc.language.isoeng
dc.publisherMDPI
dc.relation.projectIDACEX-CGL2017-87921-R
dc.rightsAtribución 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/es/
dc.subject.cdu52
dc.subject.keywordLand-surface processes
dc.subject.keywordIberian peninsula
dc.subject.keywordImpact
dc.subject.keywordSimulations
dc.subject.keywordSensitivity
dc.subject.keywordParameterization
dc.subject.keywordDeforestation
dc.subject.keywordVariability
dc.subject.keywordEvaporation
dc.subject.keywordConvection
dc.subject.ucmFísica atmosférica
dc.subject.unesco2501 Ciencias de la Atmósfera
dc.titleTemperature response to changes in vegetation fraction cover in a regional climate model
dc.typejournal article
dc.volume.number12
dspace.entity.typePublication
relation.isAuthorOfPublication552fa01a-13cf-4384-a0fa-468914cc2b06
relation.isAuthorOfPublication.latestForDiscovery552fa01a-13cf-4384-a0fa-468914cc2b06
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