Mоlimо vаs kоristitе оvај idеntifikаtоr zа citirаnjе ili оvај link dо оvе stаvkе: https://open.uns.ac.rs/handle/123456789/13319
Pоljе DC-аVrеdnоstЈеzik
dc.contributor.authorArsenić I.en
dc.contributor.authorMihailović D.en
dc.contributor.authorKapor D.en
dc.contributor.authorKallos G.en
dc.contributor.authorLalić, Bojanen
dc.contributor.authorPapadopoulos A.en
dc.date.accessioned2020-03-03T14:51:52Z-
dc.date.available2020-03-03T14:51:52Z-
dc.date.issued2000-01-01en
dc.identifier.issn0177798Xen
dc.identifier.urihttps://open.uns.ac.rs/handle/123456789/13319-
dc.description.abstractThe calculation of rocky surface temperature encounters the problem of unrealistic results due to its large changes at the interface where the energy balance equation is applied. In order to avoid this, we have modified the 'force-restore' method into a self-consistent procedure for simultaneous determination of both surface and the deep ground temperature. The approach is applicable to any celestial body where external radiation can be represented by an arbitrary periodic function. The method is tested with Earth based infrared observation on lunar surface temperature and it showed a high level of accuracy and a rather fast convergence of procedure. © Springer-Verlag 2000.en
dc.relation.ispartofTheoretical and Applied Climatologyen
dc.titleCalculating the surface temperature of the solid underlying surface by modified 'force-restore' methoden
dc.typeJournal/Magazine Articleen
dc.identifier.doi10.1007/s007040070019en
dc.identifier.scopus2-s2.0-0033764620en
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/0033764620en
dc.relation.lastpage113en
dc.relation.firstpage109en
dc.relation.issue1-2en
dc.relation.volume67en
item.fulltextNo Fulltext-
item.grantfulltextnone-
crisitem.author.deptDepartman za industrijsko inženjerstvo i menadžment-
crisitem.author.parentorgFakultet tehničkih nauka-
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