Multimodel estimate of the global terrestrial water balance: Setup and first results
International audience Six land surface models and five global hydrological models participate in a model intercomparison project [WaterModel Intercomparison Project (WaterMIP)], which for the first time compares simulation results of these different classes of models in a consistent way. In this pa...
Published in: | Journal of Hydrometeorology |
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Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2011
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Online Access: | https://hal.science/hal-01119314 https://hal.science/hal-01119314/document https://hal.science/hal-01119314/file/2011JHM1324.pdf https://doi.org/10.1175/2011JHM1324.1 |
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Open Polar |
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HAL Sorbonne Université |
op_collection_id |
ftsorbonneuniv |
language |
English |
topic |
[SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
[SDE.MCG]Environmental Sciences/Global Changes Haddeland, I. Clark, D.B. Franssen, W. Ludwig, F. Voss, F. Arnell, N.W. Bertrand, Nathalie Best, M. Folwell, S. Gerten, D. Gomes, S. Gosling, S.N. Hagemann, S. Hanasaki, N. Harding, R. Heinke, J. Kabat, P. Koirala, S. Oki, T. Polcher, Jan Stacke, T. Viterbo, P. Weedon, G.P. Yeh, P. Multimodel estimate of the global terrestrial water balance: Setup and first results |
topic_facet |
[SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience Six land surface models and five global hydrological models participate in a model intercomparison project [WaterModel Intercomparison Project (WaterMIP)], which for the first time compares simulation results of these different classes of models in a consistent way. In this paper, the simulation setup is described and aspects of the multimodel global terrestrial water balance are presented. All models were run at 0.58 spatial resolution for the global land areas for a 15-yr period (1985-99) using a newly developed global meteorological dataset. Simulated global terrestrial evapotranspiration, excluding Greenland and Antarctica, ranges from 415 to 586 mm yr -1 (from 60 000 to 85 000 km 3 yr -1), and simulated runoff ranges from 290 to 457 mm yr -1 (from 42 000 to 66 000 km 3 yr -1). Both the mean and median runoff fractions for the land surface models are lower than those of the global hydrological models, although the range is wider. Significant simulation differences between land surface and global hydrological models are found to be caused by the snow scheme employed. The physically based energy balance approach used by land surface models generally results in lower snow water equivalent values than the conceptual degreeday approach used by global hydrological models. Some differences in simulated runoff and evapotranspiration are explained by model parameterizations, although the processes included and parameterizations used are not distinct to either land surface models or global hydrological models. The results show that differences between models are a major source of uncertainty. Climate change impact studies thus need to use not only multiple climate models but also some other measure of uncertainty (e.g., multiple impact models). © 2011 American Meteorological Society. |
author2 |
Norwegian Water Resources and Energy Directorate (NVE) Wageningen University and Research Wageningen (WUR) Centre for Ecology and Hydrology, Wallingford, United Kingdom Center for Environmental Systems Research, University of Kassel, Kassel, Germany Walker Institute for Climate System Research University of Reading (UOR) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) Joint Centre for Hydro-Meteorological Research, Met Office Hadley Centre (JCHMR) United Kingdom Met Office Exeter Potsdam Institute for Climate Impact Research (PIK) Universidade de Lisboa = University of Lisbon = Université de Lisbonne (ULISBOA) University of Nottingham, UK (UON) Max Planck Institute for Meteorology (MPI-M) Max-Planck-Gesellschaft National Institute for Environmental Studies (NIES) The University of Tokyo (UTokyo) |
format |
Article in Journal/Newspaper |
author |
Haddeland, I. Clark, D.B. Franssen, W. Ludwig, F. Voss, F. Arnell, N.W. Bertrand, Nathalie Best, M. Folwell, S. Gerten, D. Gomes, S. Gosling, S.N. Hagemann, S. Hanasaki, N. Harding, R. Heinke, J. Kabat, P. Koirala, S. Oki, T. Polcher, Jan Stacke, T. Viterbo, P. Weedon, G.P. Yeh, P. |
author_facet |
Haddeland, I. Clark, D.B. Franssen, W. Ludwig, F. Voss, F. Arnell, N.W. Bertrand, Nathalie Best, M. Folwell, S. Gerten, D. Gomes, S. Gosling, S.N. Hagemann, S. Hanasaki, N. Harding, R. Heinke, J. Kabat, P. Koirala, S. Oki, T. Polcher, Jan Stacke, T. Viterbo, P. Weedon, G.P. Yeh, P. |
author_sort |
Haddeland, I. |
title |
Multimodel estimate of the global terrestrial water balance: Setup and first results |
title_short |
Multimodel estimate of the global terrestrial water balance: Setup and first results |
title_full |
Multimodel estimate of the global terrestrial water balance: Setup and first results |
title_fullStr |
Multimodel estimate of the global terrestrial water balance: Setup and first results |
title_full_unstemmed |
Multimodel estimate of the global terrestrial water balance: Setup and first results |
title_sort |
multimodel estimate of the global terrestrial water balance: setup and first results |
publisher |
HAL CCSD |
publishDate |
2011 |
url |
https://hal.science/hal-01119314 https://hal.science/hal-01119314/document https://hal.science/hal-01119314/file/2011JHM1324.pdf https://doi.org/10.1175/2011JHM1324.1 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Antarc* Antarctica Greenland |
genre_facet |
Antarc* Antarctica Greenland |
op_source |
ISSN: 1525-755X EISSN: 1525-7541 Journal of Hydrometeorology https://hal.science/hal-01119314 Journal of Hydrometeorology, 2011, 12 (5), pp.869-884. ⟨10.1175/2011JHM1324.1⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1175/2011JHM1324.1 hal-01119314 https://hal.science/hal-01119314 https://hal.science/hal-01119314/document https://hal.science/hal-01119314/file/2011JHM1324.pdf doi:10.1175/2011JHM1324.1 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1175/2011JHM1324.1 |
container_title |
Journal of Hydrometeorology |
container_volume |
12 |
container_issue |
5 |
container_start_page |
869 |
op_container_end_page |
884 |
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1802649707657297920 |
spelling |
ftsorbonneuniv:oai:HAL:hal-01119314v1 2024-06-23T07:46:58+00:00 Multimodel estimate of the global terrestrial water balance: Setup and first results Haddeland, I. Clark, D.B. Franssen, W. Ludwig, F. Voss, F. Arnell, N.W. Bertrand, Nathalie Best, M. Folwell, S. Gerten, D. Gomes, S. Gosling, S.N. Hagemann, S. Hanasaki, N. Harding, R. Heinke, J. Kabat, P. Koirala, S. Oki, T. Polcher, Jan Stacke, T. Viterbo, P. Weedon, G.P. Yeh, P. Norwegian Water Resources and Energy Directorate (NVE) Wageningen University and Research Wageningen (WUR) Centre for Ecology and Hydrology, Wallingford, United Kingdom Center for Environmental Systems Research, University of Kassel, Kassel, Germany Walker Institute for Climate System Research University of Reading (UOR) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) Joint Centre for Hydro-Meteorological Research, Met Office Hadley Centre (JCHMR) United Kingdom Met Office Exeter Potsdam Institute for Climate Impact Research (PIK) Universidade de Lisboa = University of Lisbon = Université de Lisbonne (ULISBOA) University of Nottingham, UK (UON) Max Planck Institute for Meteorology (MPI-M) Max-Planck-Gesellschaft National Institute for Environmental Studies (NIES) The University of Tokyo (UTokyo) 2011 https://hal.science/hal-01119314 https://hal.science/hal-01119314/document https://hal.science/hal-01119314/file/2011JHM1324.pdf https://doi.org/10.1175/2011JHM1324.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/2011JHM1324.1 hal-01119314 https://hal.science/hal-01119314 https://hal.science/hal-01119314/document https://hal.science/hal-01119314/file/2011JHM1324.pdf doi:10.1175/2011JHM1324.1 info:eu-repo/semantics/OpenAccess ISSN: 1525-755X EISSN: 1525-7541 Journal of Hydrometeorology https://hal.science/hal-01119314 Journal of Hydrometeorology, 2011, 12 (5), pp.869-884. ⟨10.1175/2011JHM1324.1⟩ [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2011 ftsorbonneuniv https://doi.org/10.1175/2011JHM1324.1 2024-05-30T23:53:02Z International audience Six land surface models and five global hydrological models participate in a model intercomparison project [WaterModel Intercomparison Project (WaterMIP)], which for the first time compares simulation results of these different classes of models in a consistent way. In this paper, the simulation setup is described and aspects of the multimodel global terrestrial water balance are presented. All models were run at 0.58 spatial resolution for the global land areas for a 15-yr period (1985-99) using a newly developed global meteorological dataset. Simulated global terrestrial evapotranspiration, excluding Greenland and Antarctica, ranges from 415 to 586 mm yr -1 (from 60 000 to 85 000 km 3 yr -1), and simulated runoff ranges from 290 to 457 mm yr -1 (from 42 000 to 66 000 km 3 yr -1). Both the mean and median runoff fractions for the land surface models are lower than those of the global hydrological models, although the range is wider. Significant simulation differences between land surface and global hydrological models are found to be caused by the snow scheme employed. The physically based energy balance approach used by land surface models generally results in lower snow water equivalent values than the conceptual degreeday approach used by global hydrological models. Some differences in simulated runoff and evapotranspiration are explained by model parameterizations, although the processes included and parameterizations used are not distinct to either land surface models or global hydrological models. The results show that differences between models are a major source of uncertainty. Climate change impact studies thus need to use not only multiple climate models but also some other measure of uncertainty (e.g., multiple impact models). © 2011 American Meteorological Society. Article in Journal/Newspaper Antarc* Antarctica Greenland HAL Sorbonne Université Greenland Journal of Hydrometeorology 12 5 869 884 |