Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/22901
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dc.contributor.authorRamseier, René O.-
dc.contributor.authorSander, Gary W.-
dc.date.accessioned2017-09-05T15:51:11Z-
dc.date.available2017-09-05T15:51:11Z-
dc.date.issued1966-07-
dc.identifier.urihttp://hdl.handle.net/11681/22901-
dc.description.abstractBoth the degree of sintering of snow and the rate constant as a function of temperature can be represented satisfactorily by an exponential equation. The results strongly suggest that the sintering process is one of evaporation, diffusion through the ambient temperature, and condensation.en_US
dc.language.isoenen_US
dc.publisherCold Regions Research and Engineering Laboratory (U.S.)en_US
dc.relation.ispartofseriesResearch Report;189-
dc.subjectSinteringen_US
dc.subjectSnowen_US
dc.subjectIceen_US
dc.titleTemperature dependence and mechanism of sinteringen_US
dc.typeReporten_US
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