Please use this identifier to cite or link to this item: http://ir.futminna.edu.ng:8080/jspui/handle/123456789/6782
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dc.contributor.authorShehu, Musa Danjuma-
dc.contributor.authorOlowu, R. O.-
dc.date.accessioned2021-07-06T12:49:53Z-
dc.date.available2021-07-06T12:49:53Z-
dc.date.issued2019-06-
dc.identifier.citationM. D. Shehu and R. A. Olowu (2019). Analytical Method of Land Surface Temperature Prediction, proceeding of the 2nd School of Physical Sciences Biennial International Conference on Science Technology and Innovation (SPSBIC 2019). 557 - 567en_US
dc.identifier.urihttp://repository.futminna.edu.ng:8080/jspui/handle/123456789/6782-
dc.description.abstractIn this paper, we formulated a model for the prediction of Land Surface Temperature (LST) using the Analytical Method, with the incorporation of atmospheric scale height. The following parameters were considered, meridional wind speed “v”, scale height of pressure difference “H”, coriolis force “f”, time “t”, gravitational force “g” and temperature “T”. The novelty of this study centers on the attempt to predict and analyze the behaviour of LST for a particular area using shallow water equation. The result revealed that the Land Surface Temperature increases with decrease in altitude, and this re- affirms the efficiency of Shallow Water Equation in making accurate predictions of the Land Surface Temperature.en_US
dc.language.isoenen_US
dc.publisherSchool of Physical Sciences Biennial International Conference on Science Technology and Innovationen_US
dc.relation.ispartofseriesNo. 2;557-567-
dc.subjectland surface temperatureen_US
dc.subjectzonal wind speeden_US
dc.subjectmeridional wind speeden_US
dc.subjectscale heighten_US
dc.subjectatmospheric altitudeen_US
dc.titleAnalytical Method of Land Surface Temperature Predictionen_US
dc.typeArticleen_US
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