Please use this identifier to cite or link to this item:
https://hdl.handle.net/20.500.14279/14206
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Dandou, Antant | - |
dc.contributor.author | Tombrou, M. | - |
dc.contributor.author | Akylas, Evangelos | - |
dc.contributor.author | Soulakellis, N. | - |
dc.contributor.author | Bossioli, E. | - |
dc.date.accessioned | 2019-07-01T07:08:04Z | - |
dc.date.available | 2019-07-01T07:08:04Z | - |
dc.date.issued | 2005-05-27 | - |
dc.identifier.citation | Journal of Geophysical Research D: Atmospheres, Volume 110, Issue 10, 27 May 2005, Pages 1-14 | en_US |
dc.identifier.issn | 01480227 | - |
dc.identifier.uri | https://hdl.handle.net/20.500.14279/14206 | - |
dc.description.abstract | In 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.iso | en | en_US |
dc.relation.ispartof | Journal of Geophysical Research: Atmospheres | en_US |
dc.subject | Heat island | en_US |
dc.subject | Urban climate | en_US |
dc.subject | Canopy model | en_US |
dc.title | Development and evaluation of an urban parameterization scheme in the Penn State/NCAR Mesoscale Model (MM5) | en_US |
dc.type | Article | en_US |
dc.collaboration | National and Kapodistrian University of Athens | en_US |
dc.collaboration | National Observatory of Athens | en_US |
dc.collaboration | University of Aegean | en_US |
dc.subject.category | Civil Engineering | en_US |
dc.journals | Subscription Journal | en_US |
dc.country | Greece | en_US |
dc.subject.field | Engineering and Technology | en_US |
dc.publication | Peer Reviewed | en_US |
dc.identifier.doi | 10.1029/2004JD005192 | en_US |
dc.identifier.scopus | 2-s2.0-21444450548 | - |
dc.identifier.url | https://api.elsevier.com/content/abstract/scopus_id/21444450548 | - |
cut.common.academicyear | 2004-2005 | en_US |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.fulltext | No Fulltext | - |
item.grantfulltext | none | - |
item.openairecristype | http://purl.org/coar/resource_type/c_6501 | - |
item.languageiso639-1 | en | - |
crisitem.author.dept | Department of Civil Engineering and Geomatics | - |
crisitem.author.faculty | Faculty of Engineering and Technology | - |
crisitem.author.orcid | 0000-0002-2731-657X | - |
crisitem.author.parentorg | Faculty of Engineering and Technology | - |
crisitem.journal.journalissn | 2169-8996 | - |
crisitem.journal.publisher | American Geophysical Union | - |
Appears in Collections: | Άρθρα/Articles |
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