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  4. National Symposium on Hydrology, 16-18 December 1987, Vol.- II at Roorkee
Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/3277
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dc.contributor.authorSahu, S. K.-
dc.contributor.authorSharma, S. D.-
dc.date.accessioned2019-08-02T07:34:52Z-
dc.date.available2019-08-02T07:34:52Z-
dc.date.issued1987-
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/3277-
dc.description.abstractStudies were conducted to establish an equation which would be useful in predicting evapotranspiration (ET) for upland paddy. The parameters of the equation are temperature, sunshine hour, wind velocity and relative humidity in the form of equation ET = P[(TSW/R)]x100. In order to find out the evapotranspiration, the predetermined value of P, i.e. the evapotranspiration constant is required for estimating ET. A quadratic equation (P = 0.00001772 + 0.00107045W-0.00006049W2) has been developed for estimating P following a curvilinear relationship of P with weeks of growth W.en_US
dc.language.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.subjectEvapotranspirationen_US
dc.subjectUpland Paddyen_US
dc.title28-Climatological approach for estimating evapotranspiration of upland Paddy.en_US
dc.typeTechnical Reporten_US
Appears in Collections:National Symposium on Hydrology, 16-18 December 1987, Vol.- II at Roorkee

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