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The Calculation of Solar Radiation over Lake Ontario

dc.contributor.advisorDavies, J. A.
dc.contributor.authorNunez, Manuel
dc.contributor.departmentPhysicsen_US
dc.date.accessioned2016-07-21T17:06:14Z
dc.date.available2016-07-21T17:06:14Z
dc.date.issued1971-09
dc.description.abstract<p> Simultaneous solar radiation and meteorological observations were taken from an instrumented tower located in southwestern Lake Ontario. During the four month period of this study (July-November, 1969) it was found that short-term fluxes of incoming global radiation could be predicted with a standard error which was better than 0.05 cal cm^-2min^-1 under cloudless conditions. Under cloudy conditions the lowest standard of prediction error (0.14 cal cm^-2min^-1) was obtained using a model which takes into account cloud type transmission. Under cloudless conditions the Fresnel curve underpredicts the albedos observed for low zenith angles and overpredicts when the zenith angle is high. This is mostly due to a backscatter effect estimated to be between 1.5 to 2% and to the albedo of diffuse radiation which was confirmed to be 6.5 to 7%.</p>en_US
dc.description.degreeMaster of Science (MSc)en_US
dc.description.degreetypeThesisen_US
dc.identifier.urihttp://hdl.handle.net/11375/19885
dc.language.isoen_USen_US
dc.subjectcalculation, solar radiation, Lake Ontario, meteorologicalen_US
dc.titleThe Calculation of Solar Radiation over Lake Ontarioen_US
dc.typeThesisen_US

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