Show simple item record Pomeroy, John Willard Storck, Pascal Parviainen, Jason Essery, Richard 2006-09-19T15:30:46Z 2006-09-19T15:30:46Z 2003
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
dc.identifier.issn 0894-8755
dc.identifier.other PURE: 71208
dc.identifier.other PURE UUID: 06b383ea-4abf-4bf3-9d7d-36bff3199d81
dc.identifier.other dspace: 2160/272
dc.identifier.other DSpace_20121128.csv: row: 216
dc.description Essery, R L H, Pomeroy, J W, Parvianen, J & Storck, P, Sublimation of snow from confierous forests in a climate model. Journal of Climate 16, pp 1855-1864 (2003). en
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
dc.format.extent 10 en
dc.language.iso eng
dc.relation.ispartof Journal of Climate en
dc.rights en
dc.title Sublimation of snow from confierous forests in a climate model en
dc.type /dk/atira/pure/researchoutput/researchoutputtypes/contributiontojournal/article en
dc.contributor.institution Centre for Glaciology en
dc.contributor.institution Department of Geography and Earth Sciences en
dc.description.status Peer reviewed en

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