Firn model intercomparison experiment (FirnMICE)

International audience Evolution of cold dry snow and firn plays important roles in glaciology; however, the physical formulation of a densification law is still an active research topic. We forced eight firn-densification models and one seasonal-snow model in six different experiments by imposing s...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Lundin, Jessica M.D., Stevens, C. Max, Arthern, Robert, Buizert, Christo, Orsi, Anais, Ligtenberg, Stefan R.M., Simonsen, Sebastian, Cummings, Evan, Essery, Richard, Leahy, Will, Harris, Paul, Helsen, Michiel, Waddington, Edwin
Other Authors: Department of Earth and Space Sciences Seattle, University of Washington Seattle, British Antarctic Survey (BAS), Natural Environment Research Council (NERC), College of Earth, Ocean and Atmospheric Sciences Corvallis (CEOAS), Oregon State University (OSU), Glaces et Continents, Climats et Isotopes Stables (GLACCIOS), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Institute for Marine and Atmospheric Research Utrecht (IMAU), Universiteit Utrecht / Utrecht University Utrecht, National Space Institute Lyngby (DTU Space), Danmarks Tekniske Universitet = Technical University of Denmark (DTU), University of Montana, School of Geosciences Edinburgh, University of Edinburgh (Edin.)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2017
Subjects:
Online Access:https://hal.science/hal-03226722
https://hal.science/hal-03226722/document
https://hal.science/hal-03226722/file/div-class-title-firn-model-intercomparison-experiment-firnmice-div.pdf
https://doi.org/10.1017/jog.2016.114
id ftuniparissaclay:oai:HAL:hal-03226722v1
record_format openpolar
institution Open Polar
collection Archives ouvertes de Paris-Saclay
op_collection_id ftuniparissaclay
language English
topic ice-sheet modelling
mass balance
polar firn
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
spellingShingle ice-sheet modelling
mass balance
polar firn
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
Lundin, Jessica M.D.
Stevens, C. Max
Arthern, Robert
Buizert, Christo
Orsi, Anais
Ligtenberg, Stefan R.M.
Simonsen, Sebastian
Cummings, Evan
Essery, Richard
Leahy, Will
Harris, Paul
Helsen, Michiel
Waddington, Edwin
Firn model intercomparison experiment (FirnMICE)
topic_facet ice-sheet modelling
mass balance
polar firn
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
description International audience Evolution of cold dry snow and firn plays important roles in glaciology; however, the physical formulation of a densification law is still an active research topic. We forced eight firn-densification models and one seasonal-snow model in six different experiments by imposing step changes in temperature and accumulation-rate boundary conditions; all of the boundary conditions were chosen to simulate firn densification in cold, dry environments. While the intended application of the participating models varies, they are describing the same physical system and should in principle yield the same solutions. The firn models all produce plausible depth-density profiles, but the model outputs in both steady state and transient modes differ for quantities that are of interest in ice core and altimetry research. These differences demonstrate that firn-densification models are incorrectly or incompletely representing physical processes. We quantitatively characterize the differences among the results from the various models. For example, we find depth-integrated porosity is unlikely to be inferred with confidence from a firn model to better than 2 m in steady state at a specific site with known accumulation rate and temperature. Firn Model Intercomparison Experiment can provide a benchmark of results for future models, provide a basis to quantify model uncertainties and guide future directions of firn-densification modeling.
author2 Department of Earth and Space Sciences Seattle
University of Washington Seattle
British Antarctic Survey (BAS)
Natural Environment Research Council (NERC)
College of Earth, Ocean and Atmospheric Sciences Corvallis (CEOAS)
Oregon State University (OSU)
Glaces et Continents, Climats et Isotopes Stables (GLACCIOS)
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
Institute for Marine and Atmospheric Research Utrecht (IMAU)
Universiteit Utrecht / Utrecht University Utrecht
National Space Institute Lyngby (DTU Space)
Danmarks Tekniske Universitet = Technical University of Denmark (DTU)
University of Montana
School of Geosciences Edinburgh
University of Edinburgh (Edin.)
format Article in Journal/Newspaper
author Lundin, Jessica M.D.
Stevens, C. Max
Arthern, Robert
Buizert, Christo
Orsi, Anais
Ligtenberg, Stefan R.M.
Simonsen, Sebastian
Cummings, Evan
Essery, Richard
Leahy, Will
Harris, Paul
Helsen, Michiel
Waddington, Edwin
author_facet Lundin, Jessica M.D.
Stevens, C. Max
Arthern, Robert
Buizert, Christo
Orsi, Anais
Ligtenberg, Stefan R.M.
Simonsen, Sebastian
Cummings, Evan
Essery, Richard
Leahy, Will
Harris, Paul
Helsen, Michiel
Waddington, Edwin
author_sort Lundin, Jessica M.D.
title Firn model intercomparison experiment (FirnMICE)
title_short Firn model intercomparison experiment (FirnMICE)
title_full Firn model intercomparison experiment (FirnMICE)
title_fullStr Firn model intercomparison experiment (FirnMICE)
title_full_unstemmed Firn model intercomparison experiment (FirnMICE)
title_sort firn model intercomparison experiment (firnmice)
publisher HAL CCSD
publishDate 2017
url https://hal.science/hal-03226722
https://hal.science/hal-03226722/document
https://hal.science/hal-03226722/file/div-class-title-firn-model-intercomparison-experiment-firnmice-div.pdf
https://doi.org/10.1017/jog.2016.114
genre ice core
Ice Sheet
Journal of Glaciology
genre_facet ice core
Ice Sheet
Journal of Glaciology
op_source ISSN: 0022-1430
EISSN: 1727-5652
Journal of Glaciology
https://hal.science/hal-03226722
Journal of Glaciology, 2017, 63 (239), pp.401-422. ⟨10.1017/jog.2016.114⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1017/jog.2016.114
hal-03226722
https://hal.science/hal-03226722
https://hal.science/hal-03226722/document
https://hal.science/hal-03226722/file/div-class-title-firn-model-intercomparison-experiment-firnmice-div.pdf
doi:10.1017/jog.2016.114
op_rights http://creativecommons.org/licenses/by/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1017/jog.2016.114
container_title Journal of Glaciology
container_volume 63
container_issue 239
container_start_page 401
op_container_end_page 422
_version_ 1802007692082937856
spelling ftuniparissaclay:oai:HAL:hal-03226722v1 2024-06-16T07:40:43+00:00 Firn model intercomparison experiment (FirnMICE) Lundin, Jessica M.D. Stevens, C. Max Arthern, Robert Buizert, Christo Orsi, Anais Ligtenberg, Stefan R.M. Simonsen, Sebastian Cummings, Evan Essery, Richard Leahy, Will Harris, Paul Helsen, Michiel Waddington, Edwin Department of Earth and Space Sciences Seattle University of Washington Seattle British Antarctic Survey (BAS) Natural Environment Research Council (NERC) College of Earth, Ocean and Atmospheric Sciences Corvallis (CEOAS) Oregon State University (OSU) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Institute for Marine and Atmospheric Research Utrecht (IMAU) Universiteit Utrecht / Utrecht University Utrecht National Space Institute Lyngby (DTU Space) Danmarks Tekniske Universitet = Technical University of Denmark (DTU) University of Montana School of Geosciences Edinburgh University of Edinburgh (Edin.) 2017 https://hal.science/hal-03226722 https://hal.science/hal-03226722/document https://hal.science/hal-03226722/file/div-class-title-firn-model-intercomparison-experiment-firnmice-div.pdf https://doi.org/10.1017/jog.2016.114 en eng HAL CCSD International Glaciological Society info:eu-repo/semantics/altIdentifier/doi/10.1017/jog.2016.114 hal-03226722 https://hal.science/hal-03226722 https://hal.science/hal-03226722/document https://hal.science/hal-03226722/file/div-class-title-firn-model-intercomparison-experiment-firnmice-div.pdf doi:10.1017/jog.2016.114 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0022-1430 EISSN: 1727-5652 Journal of Glaciology https://hal.science/hal-03226722 Journal of Glaciology, 2017, 63 (239), pp.401-422. ⟨10.1017/jog.2016.114⟩ ice-sheet modelling mass balance polar firn [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2017 ftuniparissaclay https://doi.org/10.1017/jog.2016.114 2024-05-17T00:05:47Z International audience Evolution of cold dry snow and firn plays important roles in glaciology; however, the physical formulation of a densification law is still an active research topic. We forced eight firn-densification models and one seasonal-snow model in six different experiments by imposing step changes in temperature and accumulation-rate boundary conditions; all of the boundary conditions were chosen to simulate firn densification in cold, dry environments. While the intended application of the participating models varies, they are describing the same physical system and should in principle yield the same solutions. The firn models all produce plausible depth-density profiles, but the model outputs in both steady state and transient modes differ for quantities that are of interest in ice core and altimetry research. These differences demonstrate that firn-densification models are incorrectly or incompletely representing physical processes. We quantitatively characterize the differences among the results from the various models. For example, we find depth-integrated porosity is unlikely to be inferred with confidence from a firn model to better than 2 m in steady state at a specific site with known accumulation rate and temperature. Firn Model Intercomparison Experiment can provide a benchmark of results for future models, provide a basis to quantify model uncertainties and guide future directions of firn-densification modeling. Article in Journal/Newspaper ice core Ice Sheet Journal of Glaciology Archives ouvertes de Paris-Saclay Journal of Glaciology 63 239 401 422