Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.14279/14206
DC FieldValueLanguage
dc.contributor.authorDandou, Antant-
dc.contributor.authorTombrou, M.-
dc.contributor.authorAkylas, Evangelos-
dc.contributor.authorSoulakellis, N.-
dc.contributor.authorBossioli, E.-
dc.date.accessioned2019-07-01T07:08:04Z-
dc.date.available2019-07-01T07:08:04Z-
dc.date.issued2005-05-27-
dc.identifier.citationJournal of Geophysical Research D: Atmospheres, Volume 110, Issue 10, 27 May 2005, Pages 1-14en_US
dc.identifier.issn01480227-
dc.identifier.urihttps://hdl.handle.net/20.500.14279/14206-
dc.description.abstractIn the present study, the Penn State/NCAR Mesoscale Model (MM5) was modified by considering recent advances in the urban boundary layer. In particular, the modifications were carried out in two directions: (1) With respect to the thermal properties of an urban surface the surface energy balance was modified by taking into account the anthropogenic heat released in urban areas and the urban heat storage term to account for urban/building mass effects, including hysteresis; and (2) the surface stress and fluxes of heat and momentum were modified following recent advances in the atmospheric boundary layer over rough surfaces under unstable conditions. The whole process was supplemented by detailed information on land use cover, derived from satellite image analysis. The modifications were applied to the high-resolution nonlocal medium-range forecast planetary boundary layer parameterization scheme, based on work by Troen and Mahrt (1986). The improvements seen with the modified model, after comparison with available measurements of temperature and fluxes, refer to (1) the strengthening of the nocturnal urban heat island; (2) the changes in the temperature, which proved to be favorable through the whole diurnal cycle, resulting in decreasing the temperature amplitude wave; (3) the decrease of turbulence and fluxes during the daytime; and (4) the diffusion coefficient and potential temperature profiles that are reduced during daytime and are increased at the lower levels during the night and thus affect accordingly the mixing height. Copyright 2005 by the American Geophysical Union.en_US
dc.language.isoenen_US
dc.relation.ispartofJournal of Geophysical Research: Atmospheresen_US
dc.subjectHeat islanden_US
dc.subjectUrban climateen_US
dc.subjectCanopy modelen_US
dc.titleDevelopment and evaluation of an urban parameterization scheme in the Penn State/NCAR Mesoscale Model (MM5)en_US
dc.typeArticleen_US
dc.collaborationNational and Kapodistrian University of Athensen_US
dc.collaborationNational Observatory of Athensen_US
dc.collaborationUniversity of Aegeanen_US
dc.subject.categoryCivil Engineeringen_US
dc.journalsSubscription Journalen_US
dc.countryGreeceen_US
dc.subject.fieldEngineering and Technologyen_US
dc.publicationPeer Revieweden_US
dc.identifier.doi10.1029/2004JD005192en_US
dc.identifier.scopus2-s2.0-21444450548-
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/21444450548-
cut.common.academicyear2004-2005en_US
item.languageiso639-1en-
item.cerifentitytypePublications-
item.fulltextNo Fulltext-
item.grantfulltextnone-
item.openairetypearticle-
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
crisitem.author.deptDepartment of Civil Engineering and Geomatics-
crisitem.author.facultyFaculty of Engineering and Technology-
crisitem.author.orcid0000-0002-2731-657X-
crisitem.author.parentorgFaculty of Engineering and Technology-
crisitem.journal.journalissn2169-8996-
crisitem.journal.publisherAmerican Geophysical Union-
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