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Article: The regional climate model REMO (v2015) coupled with the 1-D freshwater lake model FLake (v1): Fenno-Scandinavian climate and lakes

TitleThe regional climate model REMO (v2015) coupled with the 1-D freshwater lake model FLake (v1): Fenno-Scandinavian climate and lakes
Authors
Issue Date2018
Citation
Geoscientific Model Development, 2018, v. 11, n. 4, p. 1321-1342 How to Cite?
AbstractThe regional climate model REMO was coupled with the FLake lake model to include an interactive treatment of lakes. Using this new version, the Fenno-Scandinavian climate and lake characteristics were studied in a set of 35-year hindcast simulations. Additionally, sensitivity tests related to the parameterization of snow albedo were conducted. Our results show that overall the new model version improves the representation of the Fenno-Scandinavian climate in terms of 2ĝ€m temperature and precipitation, but the downside is that an existing wintertime cold bias in the model is enhanced. The lake surface water temperature, ice depth and ice season length were analyzed in detail for 10 Finnish, 4 Swedish and 2 Russian lakes and 1 Estonian lake. The results show that the model can reproduce these characteristics with reasonably high accuracy. The cold bias during winter causes overestimation of ice layer thickness, for example, at several of the studied lakes, but overall the values from the model are realistic and represent the lake physics well in a long-term simulation. We also analyzed the snow depth on ice from 10 Finnish lakes and vertical temperature profiles from 5 Finnish lakes and the model results are realistic.
Persistent Identifierhttp://hdl.handle.net/10722/349244
ISSN
2023 Impact Factor: 4.0
2023 SCImago Journal Rankings: 2.055

 

DC FieldValueLanguage
dc.contributor.authorPietikäinen, Joni Pekka-
dc.contributor.authorMarkkanen, Tiina-
dc.contributor.authorSieck, Kevin-
dc.contributor.authorJacob, Daniela-
dc.contributor.authorKorhonen, Johanna-
dc.contributor.authorRäisänen, Petri-
dc.contributor.authorGao, Yao-
dc.contributor.authorAhola, Jaakko-
dc.contributor.authorKorhonen, Hannele-
dc.contributor.authorLaaksonen, Ari-
dc.contributor.authorKaurola, Jussi-
dc.date.accessioned2024-10-17T06:57:15Z-
dc.date.available2024-10-17T06:57:15Z-
dc.date.issued2018-
dc.identifier.citationGeoscientific Model Development, 2018, v. 11, n. 4, p. 1321-1342-
dc.identifier.issn1991-959X-
dc.identifier.urihttp://hdl.handle.net/10722/349244-
dc.description.abstractThe regional climate model REMO was coupled with the FLake lake model to include an interactive treatment of lakes. Using this new version, the Fenno-Scandinavian climate and lake characteristics were studied in a set of 35-year hindcast simulations. Additionally, sensitivity tests related to the parameterization of snow albedo were conducted. Our results show that overall the new model version improves the representation of the Fenno-Scandinavian climate in terms of 2ĝ€m temperature and precipitation, but the downside is that an existing wintertime cold bias in the model is enhanced. The lake surface water temperature, ice depth and ice season length were analyzed in detail for 10 Finnish, 4 Swedish and 2 Russian lakes and 1 Estonian lake. The results show that the model can reproduce these characteristics with reasonably high accuracy. The cold bias during winter causes overestimation of ice layer thickness, for example, at several of the studied lakes, but overall the values from the model are realistic and represent the lake physics well in a long-term simulation. We also analyzed the snow depth on ice from 10 Finnish lakes and vertical temperature profiles from 5 Finnish lakes and the model results are realistic.-
dc.languageeng-
dc.relation.ispartofGeoscientific Model Development-
dc.titleThe regional climate model REMO (v2015) coupled with the 1-D freshwater lake model FLake (v1): Fenno-Scandinavian climate and lakes-
dc.typeArticle-
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.5194/gmd-11-1321-2018-
dc.identifier.scopuseid_2-s2.0-85045450819-
dc.identifier.volume11-
dc.identifier.issue4-
dc.identifier.spage1321-
dc.identifier.epage1342-
dc.identifier.eissn1991-9603-

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