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Reflection And Heating Coefficients In Southern Ontario

dc.contributor.advisorDavies, J. A.
dc.contributor.authorButtimor, Paul Henry
dc.contributor.departmentGeographyen_US
dc.date.accessioned2015-06-09T15:05:19Z
dc.date.available2015-06-09T15:05:19Z
dc.date.issued1968-10
dc.description.abstract<p> Reflection and heating coefficients were measured during the 3 month summer season at Simcoe, southern Ontario. Contrasting agricultural surfaces and atmospheric conditions were used to analyse their effect on the reflection and heating coefficients. The results confirm the postulate of Montieth (1959a) that <alpha> is close to 0.25 for many vegetated surfaces. <beta> values were positive and there was a tendency for <beta> to approximate 0.22 for many of the vegetated surfaces. Finally it was shown that the radiation balance equation for Simcoe can be generalized into a linear function of solar radiation using the same constants that are applicable to many areas in the world. </p>en_US
dc.description.degreeMaster of Arts (MA)en_US
dc.description.degreetypeThesisen_US
dc.identifier.urihttp://hdl.handle.net/11375/17487
dc.language.isoenen_US
dc.subjectReflection, heating coefficients, simcoe, Ontario, agricultural, atmospheric, postulate, Montieth, vegetated surfaces, radiation, solar radiation, simcoe horticultural experiment, crops, Budykoen_US
dc.titleReflection And Heating Coefficients In Southern Ontarioen_US
dc.typeThesisen_US

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