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The Evaporation from Three Different High-Latitude Surfaces

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dc.contributor.advisorRouse, W. R.en_US
dc.contributor.authorStewart, Bruce Roberten_US
dc.contributor.departmentGeographyen_US
dc.date.accessioned2014-06-18T17:06:56Z
dc.date.available2014-06-18T17:06:56Z
dc.date.created2009-08-17en_US
dc.date.issued1976-05en_US
dc.descriptionThis study examines the evaporation from a lichen-dominated upland ridge, a swamp and a shallow lake in the Hudson Bay lowlands evaluated by the energy-budget and equilibrium model approaches. Energy-budget calculations reveal that on average 54, 66 and 55 percent of the daily net radiation is utilized in the evaporative process over the ridge, swamp and lake surfaces respectively. For the ridge half-hourly and daily values of evaporation were approximated closely by equilibrium estimates, while for the other surfaces close approximation was achieved by the Priestley and Taylor (1972) model where the ratio of actual to equilibrium evaporation equals 1.26. A simple model, expressed in terms of incoming solar radiation and the screen height air temperature, is developed for each surface from the comparison of actual to equilibrium evaporation. Tests of the models at different locations indicate that the actual evaporation can be estimated on a daily basis within 6 percent for dry upland and saturated lowland swamp surfaces, while for shallow lakes, the evaporation can be determined within 10 percent over periods of two weeks.en_US
dc.description.abstracten_US
dc.description.degreeDoctor of Philosophy (PhD)en_US
dc.identifier.otheropendissertations/916en_US
dc.identifier.other1682en_US
dc.identifier.other945005en_US
dc.identifier.urihttp://hdl.handle.net/11375/14272
dc.subjectGeographyen_US
dc.subjectGeographyen_US
dc.titleThe Evaporation from Three Different High-Latitude Surfacesen_US
dc.typethesisen_US

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