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dc.contributor.author John W. en_US
dc.contributor.author Pascal en_US
dc.contributor.author Jason en_US
dc.contributor.author Richard en_US
dc.date.accessioned 2006-09-19T15:30:46Z
dc.date.available 2006-09-19T15:30:46Z
dc.date.issued 2003 en_US
dc.identifier.citation Pomeroy , J W , Storck , P , Parviainen , J & Essery , R 2003 , ' Sublimation of snow from confierous forests in a climate model ' Journal of Climate , pp. 1855-1864 . en_US
dc.identifier.other PURE: 71208 en_US
dc.identifier.other dspace: 2160/272 en_US
dc.identifier.uri http://hdl.handle.net/2160/272
dc.description.abstract Improved representations of snow interception by coniferous forest canopies and sublimation of intercepted snow are implemented in a land-surface model. Driven with meteorological observations from forested sites in Canada, the USA and Sweden, the modified model is found to give reduced sublimation, better simulations of snow loads on and below canopies, and improved predictions of snowmelt runoff. When coupled to an atmospheric model in a GCM, however, drying and warming of the air because of the reduced sublimation provides a feedback which limits the impact of the new canopy snow model on the predicted sublimation. There is little impact on the average annual snowmelt runoff in the GCM, but runoff is delayed and peak runoff increased by the introduction of the canopy snow model. en_US
dc.format.extent 10 en_US
dc.relation.ispartof Journal of Climate en_US
dc.title Sublimation of snow from confierous forests in a climate model en_US
dc.contributor.pbl Aberystwyth University en_US
dc.contributor.pbl Centre for Glaciology en_US


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