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dc.contributor.authorEasterling, David R.
dc.contributor.authorGoodge, Grant
dc.contributor.authorMenne, Matthew J.
dc.contributor.authorWilliams, Claude N.
dc.contributor.authorLevinson, David
dc.date.accessioned2017-06-09T16:46:57Z
dc.date.available2017-06-09T16:46:57Z
dc.date.copyright2005/12/01
dc.date.issued2005
dc.identifier.otherams-73974.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4216147
dc.description.abstractTemperature time series for stations in western North Carolina are used to evaluate the potential for an urban signal in the local temperature trend, and to compare a homogeneous temperature record from a mountain-top station to two versions of the lower-tropospheric, satellite-derived temperatures from the Microwave Sounding Unit (MSU). Results regarding the urban signal are in agreement with the conclusion from previous investigations that after a location is urbanized, the local temperature trend is consistent with trends derived from surrounding, more rural stations. With respect to the mountain top and lower-tropospheric temperature comparison, the magnitudes of the two MSU-derived trends for the western North Carolina area are closer to the average annual minimum temperature trend than to the annual average maximum temperature trend.
dc.publisherAmerican Meteorological Society
dc.titleA Comparison of Local and Regional Trends in Surface and Lower-Tropospheric Temperatures in Western North Carolina
dc.typeJournal Paper
dc.journal.volume9
dc.journal.issue28
dc.journal.titleEarth Interactions
dc.identifier.doi10.1175/EI161.1
dc.journal.fristpage1
dc.journal.lastpage9
dc.treeEarth Interactions:;2005:;volume( 009 ):;issue: 028
dc.contenttypeFulltext


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