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Comparative study of evapotranspiration variation and its relationship with other climatic parameters in Asaba and Uyo

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dc.contributor.author Umego, Okwunna M.
dc.contributor.author Ewemoje, Temitayo A.
dc.contributor.author Ilesanmi, Oluwaseun A.
dc.date.accessioned 2020-12-21T15:15:37Z
dc.date.available 2020-12-21T15:15:37Z
dc.date.issued 2018-09-02
dc.identifier.issn 23105496
dc.identifier.uri http://hdl.handle.net/123456789/4435
dc.description 7p:, ill. en_US
dc.description.abstract This study was carried out to assess the variations of Reference Evapotranspiration (ETO also denoted with RET) calculated using FAO-56 Penman Monteith model of two locations Asaba and Uyo and evaluate its relationships with the variations of other climatic parameters. Meteorological data of forty one years (1975-2015) and thirty five years (1981-2015) period for Asaba and Uyo, respectively gotten from Nigeria Meteorological Agency, Abuja were used. It was observed that the variations of Evapotranspiration (ET) in both locations were in line with two seasons (rainy and dry) normally experienced in Nigeria having its highest value in March (4.8 mm/day) for Asaba and for Uyo in February (4.5 mm/day); and its lowest value in August (3.1 mm/day) for Asaba and in July (2.9 mm/day) for Uyo. ET variation when compared with other climatic variables in both locations was observed to have the same trend with maximum temperature, solar radiation and sunshine hours. It also has the same variation with minimum temperature though with slight deviation. It was observed that ET variation is inversely proportional to the variation relative humidity. Wind speed displayed relatively small variation in its trend over the study period and is not in line with the variations of ET en_US
dc.language.iso en en_US
dc.publisher University of Cape Coast en_US
dc.subject Evapotranspiration en_US
dc.subject Climatic Variables en_US
dc.subject FAO Penman-Monteith Model en_US
dc.subject Variations en_US
dc.title Comparative study of evapotranspiration variation and its relationship with other climatic parameters in Asaba and Uyo en_US
dc.type Article en_US


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