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dc.contributor.authorScheitlin, Kelsey
dc.date.accessioned2017-06-09T16:41:22Z
dc.date.available2017-06-09T16:41:22Z
dc.date.copyright2013/10/01
dc.date.issued2013
dc.identifier.otherams-72267.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214251
dc.description.abstracthis study analyzes the influence of the Atlantic Ocean and Chesapeake Bay on the diurnal temperature range (DTR) reported by nearby weather stations. Coastal locations reported the smallest DTRs and DTR fluctuations, and DTR increased with distance from the ocean. Month of the year and airmass type also proved to be significant predictors of DTR. All locations showed a bimodal annual DTR pattern with peaks during the transitional seasons and experienced the greatest DTR during dry and/or warm air masses. Proximity to the ocean had the largest (smallest) influence on DTR during dry (moist) air masses with extreme (moderate) temperatures. Seasonally, the proximity to the ocean had the strongest impact on DTR during early?middle spring. A multiple regression model using distance from water, month, and airmass type explains over 30% of DTR variability in the area (p < 0.01). Airmass type has the largest influence on DTR, and changes in both air mass and month impacted the DTR of continental locations more than coastal locations. Land use, cloud cover, and wind speed/direction are additional variables that could account for differences not explained by the model.
dc.publisherAmerican Meteorological Society
dc.titleThe Maritime Influence on Diurnal Temperature Range in the Chesapeake Bay Area
dc.typeJournal Paper
dc.journal.volume17
dc.journal.issue21
dc.journal.titleEarth Interactions
dc.identifier.doi10.1175/2013EI000546.1
dc.journal.fristpage1
dc.journal.lastpage14
dc.treeEarth Interactions:;2013:;volume( 017 ):;issue: 021
dc.contenttypeFulltext


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