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dc.creatorMcCloskey, John W.en_US
dc.date.accessioned2006-07-07T02:16:52Z
dc.date.available2006-07-07T02:16:52Z
dc.date.issued1986-03en_US
dc.identifier.citationThe Ohio Journal of Science. v86, n1 (March, 1986), 8-10en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/23111
dc.descriptionAuthor Institution: Department of Mathematics, University of Daytonen_US
dc.description.abstractA sinusoidal temperature model has been developed which describes maximum and minimum temperature patterns through a yearly cycle for the major cities in and around the state of Ohio. Thirty-year monthly means provide the basis for the calculation of model parameters that are used to analytically compare temperature patterns among the selected cities. An amplitude of 11.8°C for the minimum temperature cycle in Columbus implies that the average minimum temperature for January in this city was 23.6°C colder than the average summer minimum temperature for July. Larger amplitudes for the maximum temperature cycles imply a larger difference between average summer daily extremes than for average winter daily extremes. With minimum winter temperatures well below freezing over the state, the model indicates a period of over 100 days during winter where the average minimum daily temperatures are below 0°C.en_US
dc.format.extent338930 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.titleSeasonal Temperature Patterns of Selected Cities in and Around Ohioen_US


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