Show simple item record Pattyn, F. Perichon, L. Aschwanden, A. Breuer, B. de Smedt, B. Gagliardini, O. Gudmundsson, G. H. Hindmarsh, R. C. Hubbard, Alun Lloyd Johnson, J. V. Kleiner, T. Konovalov, Y. Martin, C. Payne, A. J. Pollard, D. Price, S. Rückamp, M. Saito, F. Souček, O. Sugiyama, S. Zwinger, T. 2011-06-27T11:07:51Z 2011-06-27T11:07:51Z 2008-08-26
dc.identifier.citation Pattyn , F , Perichon , L , Aschwanden , A , Breuer , B , de Smedt , B , Gagliardini , O , Gudmundsson , G H , Hindmarsh , R C , Hubbard , A L , Johnson , J V , Kleiner , T , Konovalov , Y , Martin , C , Payne , A J , Pollard , D , Price , S , Rückamp , M , Saito , F , Souček , O , Sugiyama , S & Zwinger , T 2008 , ' Benchmark experiments for higher-order and full-Stokes ice sheet models (ISMIP-HOM) ' Cryosphere , vol 2 , no. 95-108 , pp. 95-108 . DOI: 10.5194/tc-2-95-2008 en
dc.identifier.issn 1994-0416
dc.identifier.other PURE: 168407
dc.identifier.other PURE UUID: 6f3eb49c-f377-42a5-b32d-023ad08c212b
dc.identifier.other dspace: 2160/7108
dc.identifier.other DSpace_20121128.csv: row: 4354
dc.identifier.other RAD: 3616
dc.identifier.other RAD_Outputs_All_ID_Import_20121105.csv: row: 1598
dc.identifier.other Scopus: 50949109429
dc.description Pattyn, F., Perichon, L., Aschwanden, A., Breuer, B., de Smedt, B., Gagliardini, O., Gudmundsson, G. H., Hindmarsh, R. C. A., Hubbard, A. L., Johnson, J. V., Kleiner, T. et al. (2008). Benchmark experiments for higher-order and full-Stokes ice sheet models (ISMIP-HOM). Cryosphere, 2, (2), 95-108. en
dc.description.abstract We present the results of the first ice sheet model intercomparison project for higher-order and full-Stokes ice sheet models. These models are compared and verified in a series of six experiments of which one has an analytical solution obtained from a perturbation analysis. The experiments are applied to both 2-D and 3-D geometries; five experiments are steady-state diagnostic, and one has a time-dependent prognostic solution. All participating models give results that are in close agreement. A clear distinction can be made between higher-order models and those that solve the full system of equations. The full-Stokes models show a much smaller spread, hence are in better agreement with one another and with the analytical solution. en
dc.format.extent 14 en
dc.language.iso eng
dc.relation.ispartof Cryosphere en
dc.rights en
dc.title Benchmark experiments for higher-order and full-Stokes ice sheet models (ISMIP-HOM) en
dc.type /dk/atira/pure/researchoutput/researchoutputtypes/contributiontojournal/article en
dc.description.version publishersversion en
dc.contributor.institution Department of Geography and Earth Sciences en
dc.description.status Peer reviewed en

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