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dc.contributor.authorLaramie, Richard L.en_US
dc.contributor.authorSchaake, Jr., John C.en_US
dc.date.accessioned2022-06-13T13:06:19Z
dc.date.available2022-06-13T13:06:19Z
dc.date.issued1972-01
dc.identifier143
dc.identifier.urihttps://hdl.handle.net/1721.1/142971
dc.descriptionThe work upon which this publication is based was supported by the Subsecretar�a de Recursos H�dricos, Ministerio de Obras y Servicios P�blicos, Argentina.en_US
dc.description.abstractThe efficient design of many water management projects requires the ability to predict the time distribution of runoff from a melting snowfield. A continuous model of the snow accumation and melting processes is presented for this purpose. The empirical and theoretical equations that have been used to represent these processes are integrated into a model developed to have a wide range of applicability owing to its flexible data requirements. The snowmelt model is tested using various combinations of recorded data thought likely to be available in practical design problems. A comparison of the generated values of certain important snowpack variables with those actually observed shows good agreement. Application of the model to an experimental catchment is made to estimate streamflows resulting from the computed snowmelt. Although the results were favorable, suggestions are made as to how they may be improved.en_US
dc.publisherCambridge Ralph M. Parsons Laboratory for Water Resources and Hydrodynamics, Massachusetts Institute of Technology
dc.relation.ispartofseriesR (Massachusetts Institute of Technology. Department of Civil Engineering) ; 72-7.
dc.relation.ispartofseriesReport (Ralph M. Parsons Laboratory for Water Resources and Hydrodynamics) ; 143.
dc.titleSimulation of the Continuous Snowmelt Processen_US
dc.identifier.oclc1733790
dc.identifier.aleph246392


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