Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/3634
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dc.contributor.authorMishra, S. K.-
dc.contributor.authorRawat, Soban Singh-
dc.contributor.authorPandey, R. P.-
dc.contributor.authorChakraborty, Shiulee-
dc.contributor.authorJain, M. K.-
dc.contributor.authorChaube, U. C.-
dc.date.accessioned2019-09-25T09:50:44Z-
dc.date.available2019-09-25T09:50:44Z-
dc.date.issued2014-
dc.identifier.citationJ. Hydrol. Eng. 2014.19:355-365en_US
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/3634-
dc.description.abstractThis paper presents a relationship between the runoff curve number (CN) and mean potential evapotranspiration (PET) using longterm daily rainfall-runoff data. To this end, CNs were derived for different durations from rainfall-runoff data of eight different agro-climatic river basins in India, and these were correlated with PET derived for respective watersheds using the standard Penman-Monteith method. The resulting high coefficient of determination (R2) values, viz, 0.99 for Hemawati and Mohegoan; 0.98 for Haridanagar, Kalu, and Seonath; 0.96 for Manot, Ghodahadho, and Ramganga strongly support the versatility of the derived relationship. This relationship also invokes determination of PET from the available published CN values, and therefore may be quite useful in field applications.en_US
dc.language.isoenen_US
dc.publisherASCEen_US
dc.subjectCurve numberen_US
dc.subjectNational Engineering Handbook hydrology (NEH-4); Penman-Monteith; Potential evapotranspiration (PET); Soil conservation service; Water balanceen_US
dc.subjectPenman-Monteithen_US
dc.subjectPotential evapotranspiration (PET)en_US
dc.subjectSoil conservation serviceen_US
dc.subjectWater balanceen_US
dc.titleRelationship between Runoff Curve Number and PETen_US
dc.typeArticleen_US
Appears in Collections:Research papers in International Journals

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