28-Climatological approach for estimating evapotranspiration of upland Paddy.

dc.contributor.author	Sahu, S. K.
dc.contributor.author	Sharma, S. D.
dc.date.accessioned	2019-08-02T07:34:52Z
dc.date.available	2019-08-02T07:34:52Z
dc.date.issued	1987
dc.identifier.uri	http://117.252.14.250:8080/jspui/handle/123456789/3277
dc.description.abstract	Studies 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.iso	en	en_US
dc.publisher	National Institute of Hydrology	en_US
dc.subject	Evapotranspiration	en_US
dc.subject	Upland Paddy	en_US
dc.title	28-Climatological approach for estimating evapotranspiration of upland Paddy.	en_US
dc.type	Technical Report	en_US