Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/5872
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dc.contributor.authorColbeck, Samuel C.-
dc.date.accessioned2016-03-21T21:09:03Z-
dc.date.available2016-03-21T21:09:03Z-
dc.date.issued1973-09-
dc.identifier.urihttp://hdl.handle.net/11681/5872-
dc.descriptionResearch Report-
dc.descriptionAbstract: The flow of water through layered snowpacks is discussed. A method for predicting flow through unsaturated layers is given. The flow along ice layers and through ice layers is analyzed in terms of the slope, permeability, thickness and length of the layers. It is shown that the permeability of ice layers required to cause large flow diversions is quite small. The effect of slope is large even at small angles.-
dc.publisherCold Regions Research and Engineering Laboratory (U.S.)-
dc.publisherEngineer Research and Development Center (U.S.)-
dc.relationhttp://acwc.sdp.sirsi.net/client/en_US/search/asset/1014500-
dc.relation.ispartofseriesResearch report (Cold Regions Research and Engineering Laboratory (U.S.)) ; 311.-
dc.rightsApproved for public release; distribution is unlimited.-
dc.sourceThis Digital Resource was created from scans of the Print Resource-
dc.subjectDrainage-
dc.subjectGravitational water-
dc.subjectHydrology-
dc.subjectHydrodynamics-
dc.subjectPermeability-
dc.subjectIce-
dc.subjectPercolation-
dc.subjectSnow-
dc.subjectSnow cover-
dc.subjectSnowmelt-
dc.subjectSurface water runoff-
dc.titleEffects of stratigraphic layers on water flow through snow-
dc.typeDOCUMENT-
Appears in Collections:CRREL Research Report

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