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dc.contributor.authorNitter, Marianne
dc.date.accessioned2012-11-15T13:24:05Z
dc.date.available2012-11-15T13:24:05Z
dc.date.issued2009
dc.identifier.citationNitter, M. (2009) Klimarom : klimaets avhengighet av skala og landskap. In Nitter, M. og Pedersen, E.S (red.) Tverrfaglige perspektiver. Stavanger : Arkeologisk museum i Stavangerno_NO
dc.identifier.urihttp://hdl.handle.net/11250/181456
dc.description.abstractVariations in temperature, precipitation and wind depend on variations in topography, vegetation, surface properties and topographic lines in a given landscape. Various weather phenomena exist within well-defined areas, called climate-spaces in this article. A climate-space is defined as an area where the climate is homogenous or uniform in relation to a specific climatic parameter (e.g. temperature, precipitation, wind direction or wind force). The area of a climate-space is limited by topography and vegetation. The term climate-space is introduced for its ability to convey abstract physico-meteorological phenomena to archaeological parlance and terminology, thereby attaining a common terminological platform for dialogue. Climate-space may exist on four steps or levels: micro, local, meso and macro. In this article climate-space is considered in relation to 1) weather phenomena limited in time, 2) the actual climatic parameter, and 3) the topographic lines in a given landscape. Additional examples of weather phenomena within each category of climate-space are given.no_NO
dc.language.isonobno_NO
dc.publisherArkeologisk Museum i Stavangerno_NO
dc.relation.ispartofseriesAmS-Varia;49
dc.subjectarkeologino_NO
dc.subjectklimano_NO
dc.subjectværno_NO
dc.titleKlimarom : klimaets avhengighet av skala og landskapno_NO
dc.typeChapterno_NO
dc.typePeer reviewedno_NO
dc.subject.nsiVDP::Humanities: 000::Archeology: 090::Nordic archeology: 091no_NO


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