The future of sea ice modelling: where do we go from here?

Continuum sea ice models have been applied close to the presumed limits of their validity for many years, yet they remain compatible with current observations. The resolution requirements for sea ice models varies considerably depending on the application (e.g., large ensembles, paleoclimate simulat...

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Published in:Bulletin of the American Meteorological Society
Main Authors: Blockley, E., Vancoppenolle, M., Hunke, E., Bitz, C., Feltham, D., Lemieux, J., Losch, M., Maisonnave, E., Notz, D., Rampal, P., Tietsche, S., Tremblay, B., Turner, A., Massonnet, F., Ólason, E., Roberts, A., Aksenov, Y., Fichefet, T., Garric, G., Iovino, D., Madec, G., Rousset, C., Salas y Melia, D., Schroeder, D.
Format: Conference Object
Language:English
Published: 2020
Subjects:
Online Access:http://hdl.handle.net/21.11116/0000-0006-88F4-D
http://hdl.handle.net/21.11116/0000-0007-AFFB-A
http://hdl.handle.net/21.11116/0000-0007-AFFC-9
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spelling ftpubman:oai:pure.mpg.de:item_3237314 2023-08-27T04:11:52+02:00 The future of sea ice modelling: where do we go from here? Blockley, E. Vancoppenolle, M. Hunke, E. Bitz, C. Feltham, D. Lemieux, J. Losch, M. Maisonnave, E. Notz, D. Rampal, P. Tietsche, S. Tremblay, B. Turner, A. Massonnet, F. Ólason, E. Roberts, A. Aksenov, Y. Fichefet, T. Garric, G. Iovino, D. Madec, G. Rousset, C. Salas y Melia, D. Schroeder, D. 2020-08 application/pdf http://hdl.handle.net/21.11116/0000-0006-88F4-D http://hdl.handle.net/21.11116/0000-0007-AFFB-A http://hdl.handle.net/21.11116/0000-0007-AFFC-9 eng eng info:eu-repo/grantAgreement/EC/H2020/824084 info:eu-repo/semantics/altIdentifier/doi/10.1175/BAMS-D-20-0073.1 http://hdl.handle.net/21.11116/0000-0006-88F4-D http://hdl.handle.net/21.11116/0000-0007-AFFB-A http://hdl.handle.net/21.11116/0000-0007-AFFC-9 info:eu-repo/semantics/openAccess Bulletin of the American Meteorological Society info:eu-repo/semantics/conferenceObject 2020 ftpubman https://doi.org/10.1175/BAMS-D-20-0073.1 2023-08-02T00:38:22Z Continuum sea ice models have been applied close to the presumed limits of their validity for many years, yet they remain compatible with current observations. The resolution requirements for sea ice models varies considerably depending on the application (e.g., large ensembles, paleoclimate simulations, short-range forecasting), and therefore continuum models will likely remain useful for many years to come. Meanwhile, it is highly desirable to explore the potential of DEMs. These models are expected to be more physically faithful at the highest resolutions envisioned for sea ice in ESMs, provided they incorporate all the required processes. DEMs may also prove more efficient for some new computer architectures. Such perspectives highlight the need for the sea ice modeling community to have a clear and consistent vision of the future evolution of HPC systems. Sea ice models are used for many different purposes and therefore benefit from modularity, which allows the activation or exclusion of parameterizations and code features. Thus, users can adjust model complexity to fit their specific application. Considering limited human resources among core sea ice modeling groups, engagement of the wider community has proven a very efficient way to advance large-scale sea ice models. However, there is still scope for further integration of the wider community in model development activities. An important feature of the Laugarvatn sea ice modeling workshop was the open minded atmosphere in which very different views were exchanged. The workshop successfully brought together model developers and users of sea ice models for Earth system modeling, operational forecasting and (re)analyses. International sea ice modeling workshops such as this foster collaboration and community engagement in the field of sea ice modeling. A recommendation from this workshop is that the exercise should be repeated every 2-3 years to maintain community engagement, exchange cutting-edge ideas, and reinforce collaborative momentum. © 2020 ... Conference Object Sea ice Max Planck Society: MPG.PuRe Laugarvatn ENVELOPE(-20.711,-20.711,64.210,64.210) Bulletin of the American Meteorological Society 101 8 E1304 E1311
institution Open Polar
collection Max Planck Society: MPG.PuRe
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description Continuum sea ice models have been applied close to the presumed limits of their validity for many years, yet they remain compatible with current observations. The resolution requirements for sea ice models varies considerably depending on the application (e.g., large ensembles, paleoclimate simulations, short-range forecasting), and therefore continuum models will likely remain useful for many years to come. Meanwhile, it is highly desirable to explore the potential of DEMs. These models are expected to be more physically faithful at the highest resolutions envisioned for sea ice in ESMs, provided they incorporate all the required processes. DEMs may also prove more efficient for some new computer architectures. Such perspectives highlight the need for the sea ice modeling community to have a clear and consistent vision of the future evolution of HPC systems. Sea ice models are used for many different purposes and therefore benefit from modularity, which allows the activation or exclusion of parameterizations and code features. Thus, users can adjust model complexity to fit their specific application. Considering limited human resources among core sea ice modeling groups, engagement of the wider community has proven a very efficient way to advance large-scale sea ice models. However, there is still scope for further integration of the wider community in model development activities. An important feature of the Laugarvatn sea ice modeling workshop was the open minded atmosphere in which very different views were exchanged. The workshop successfully brought together model developers and users of sea ice models for Earth system modeling, operational forecasting and (re)analyses. International sea ice modeling workshops such as this foster collaboration and community engagement in the field of sea ice modeling. A recommendation from this workshop is that the exercise should be repeated every 2-3 years to maintain community engagement, exchange cutting-edge ideas, and reinforce collaborative momentum. © 2020 ...
format Conference Object
author Blockley, E.
Vancoppenolle, M.
Hunke, E.
Bitz, C.
Feltham, D.
Lemieux, J.
Losch, M.
Maisonnave, E.
Notz, D.
Rampal, P.
Tietsche, S.
Tremblay, B.
Turner, A.
Massonnet, F.
Ólason, E.
Roberts, A.
Aksenov, Y.
Fichefet, T.
Garric, G.
Iovino, D.
Madec, G.
Rousset, C.
Salas y Melia, D.
Schroeder, D.
spellingShingle Blockley, E.
Vancoppenolle, M.
Hunke, E.
Bitz, C.
Feltham, D.
Lemieux, J.
Losch, M.
Maisonnave, E.
Notz, D.
Rampal, P.
Tietsche, S.
Tremblay, B.
Turner, A.
Massonnet, F.
Ólason, E.
Roberts, A.
Aksenov, Y.
Fichefet, T.
Garric, G.
Iovino, D.
Madec, G.
Rousset, C.
Salas y Melia, D.
Schroeder, D.
The future of sea ice modelling: where do we go from here?
author_facet Blockley, E.
Vancoppenolle, M.
Hunke, E.
Bitz, C.
Feltham, D.
Lemieux, J.
Losch, M.
Maisonnave, E.
Notz, D.
Rampal, P.
Tietsche, S.
Tremblay, B.
Turner, A.
Massonnet, F.
Ólason, E.
Roberts, A.
Aksenov, Y.
Fichefet, T.
Garric, G.
Iovino, D.
Madec, G.
Rousset, C.
Salas y Melia, D.
Schroeder, D.
author_sort Blockley, E.
title The future of sea ice modelling: where do we go from here?
title_short The future of sea ice modelling: where do we go from here?
title_full The future of sea ice modelling: where do we go from here?
title_fullStr The future of sea ice modelling: where do we go from here?
title_full_unstemmed The future of sea ice modelling: where do we go from here?
title_sort future of sea ice modelling: where do we go from here?
publishDate 2020
url http://hdl.handle.net/21.11116/0000-0006-88F4-D
http://hdl.handle.net/21.11116/0000-0007-AFFB-A
http://hdl.handle.net/21.11116/0000-0007-AFFC-9
long_lat ENVELOPE(-20.711,-20.711,64.210,64.210)
geographic Laugarvatn
geographic_facet Laugarvatn
genre Sea ice
genre_facet Sea ice
op_source Bulletin of the American Meteorological Society
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container_title Bulletin of the American Meteorological Society
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