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RN-16 : Estimation of evapotranspiration for variable water table situations

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dc.contributor.author Soni, B.
dc.contributor.author Mishra, G. C.
dc.date.accessioned 2019-06-03T04:36:42Z
dc.date.available 2019-06-03T04:36:42Z
dc.date.issued 1985
dc.identifier.uri http://117.252.14.250:8080/xmlui/handle/123456789/2801
dc.description.abstract Many investigators have studied rates of evaporation from soils where water table is at shallow depth. The rate of evaporation may be controlled by either the capacity of the atmospheric environment to evaporate water or the capacity of the soil to transmit water to the surface. A review note has been prepared which gives in detail the methods for estimation of evapotranspiration which considers both the soil properties and meteorological factors. The evaporation rate decreases with water table depth more steeply in coarse textured soil than in fine textured soils. en_US
dc.language.iso en en_US
dc.publisher National Institute of Hydrology en_US
dc.relation.ispartofseries ;RN-16
dc.subject Estimation of evapotranspiration en_US
dc.subject evapotranspiration for variable water table en_US
dc.subject Evapotranspiration en_US
dc.title RN-16 : Estimation of evapotranspiration for variable water table situations en_US
dc.type Technical Report en_US


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