The Tuning Strategy of IPSL‐CM6A‐LR

Abstract The assessment of current and future risks for natural and human systems associated with climate change largely relies on numerical simulations performed with state‐of‐the‐art climate models. Various steps are involved in the development of such models, from development of individual compon...

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Autores principales: Juliette Mignot, Frédéric Hourdin, Julie Deshayes, Olivier Boucher, Guillaume Gastineau, Ionela Musat, Martin Vancoppenolle, Jérôme Servonnat, Arnaud Caubel, Frédérique Chéruy, Sébastien Denvil, Jean‐Louis Dufresne, Christian Ethé, Laurent Fairhead, Marie‐Alice Foujols, Jean‐Yves Grandpeix, Guillaume Levavasseur, Olivier Marti, Matthew Menary, Catherine Rio, Clément Rousset, Yona Silvy
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Publicado: American Geophysical Union (AGU) 2021
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spelling oai:doaj.org-article:d0feb0d749634f6e8523a8c964ccf73c2021-11-24T08:11:41ZThe Tuning Strategy of IPSL‐CM6A‐LR1942-246610.1029/2020MS002340https://doaj.org/article/d0feb0d749634f6e8523a8c964ccf73c2021-05-01T00:00:00Zhttps://doi.org/10.1029/2020MS002340https://doaj.org/toc/1942-2466Abstract The assessment of current and future risks for natural and human systems associated with climate change largely relies on numerical simulations performed with state‐of‐the‐art climate models. Various steps are involved in the development of such models, from development of individual components of the climate system up to free parameter calibration of the fully coupled model. Here, we describe the final tuning phase for the IPSL‐CM6A‐LR climate model. This phase alone lasted more than 3 years and relied on several pillars: (i) the tuning against present‐day conditions given a small adjustment of the ocean surface albedo to compensate for the current oceanic heat uptake, (ii) the release of successive versions after adjustments of the individual components, implying a systematic and recurrent adjustment of the atmospheric energetics, and (iii) the use of a few metrics based on large scale variables such as near‐global mean temperature, summer Arctic sea‐ice extent, as targets for the tuning. Successes, lessons and prospects of this tuning strategy are discussed.Juliette MignotFrédéric HourdinJulie DeshayesOlivier BoucherGuillaume GastineauIonela MusatMartin VancoppenolleJérôme ServonnatArnaud CaubelFrédérique ChéruySébastien DenvilJean‐Louis DufresneChristian EthéLaurent FairheadMarie‐Alice FoujolsJean‐Yves GrandpeixGuillaume LevavasseurOlivier MartiMatthew MenaryCatherine RioClément RoussetYona SilvyAmerican Geophysical Union (AGU)articleatmospheric energetic adjustmentcalibrationclimate model tuningmetricspresent‐day controlPhysical geographyGB3-5030OceanographyGC1-1581ENJournal of Advances in Modeling Earth Systems, Vol 13, Iss 5, Pp n/a-n/a (2021)
institution DOAJ
collection DOAJ
language EN
topic atmospheric energetic adjustment
calibration
climate model tuning
metrics
present‐day control
Physical geography
GB3-5030
Oceanography
GC1-1581
spellingShingle atmospheric energetic adjustment
calibration
climate model tuning
metrics
present‐day control
Physical geography
GB3-5030
Oceanography
GC1-1581
Juliette Mignot
Frédéric Hourdin
Julie Deshayes
Olivier Boucher
Guillaume Gastineau
Ionela Musat
Martin Vancoppenolle
Jérôme Servonnat
Arnaud Caubel
Frédérique Chéruy
Sébastien Denvil
Jean‐Louis Dufresne
Christian Ethé
Laurent Fairhead
Marie‐Alice Foujols
Jean‐Yves Grandpeix
Guillaume Levavasseur
Olivier Marti
Matthew Menary
Catherine Rio
Clément Rousset
Yona Silvy
The Tuning Strategy of IPSL‐CM6A‐LR
description Abstract The assessment of current and future risks for natural and human systems associated with climate change largely relies on numerical simulations performed with state‐of‐the‐art climate models. Various steps are involved in the development of such models, from development of individual components of the climate system up to free parameter calibration of the fully coupled model. Here, we describe the final tuning phase for the IPSL‐CM6A‐LR climate model. This phase alone lasted more than 3 years and relied on several pillars: (i) the tuning against present‐day conditions given a small adjustment of the ocean surface albedo to compensate for the current oceanic heat uptake, (ii) the release of successive versions after adjustments of the individual components, implying a systematic and recurrent adjustment of the atmospheric energetics, and (iii) the use of a few metrics based on large scale variables such as near‐global mean temperature, summer Arctic sea‐ice extent, as targets for the tuning. Successes, lessons and prospects of this tuning strategy are discussed.
format article
author Juliette Mignot
Frédéric Hourdin
Julie Deshayes
Olivier Boucher
Guillaume Gastineau
Ionela Musat
Martin Vancoppenolle
Jérôme Servonnat
Arnaud Caubel
Frédérique Chéruy
Sébastien Denvil
Jean‐Louis Dufresne
Christian Ethé
Laurent Fairhead
Marie‐Alice Foujols
Jean‐Yves Grandpeix
Guillaume Levavasseur
Olivier Marti
Matthew Menary
Catherine Rio
Clément Rousset
Yona Silvy
author_facet Juliette Mignot
Frédéric Hourdin
Julie Deshayes
Olivier Boucher
Guillaume Gastineau
Ionela Musat
Martin Vancoppenolle
Jérôme Servonnat
Arnaud Caubel
Frédérique Chéruy
Sébastien Denvil
Jean‐Louis Dufresne
Christian Ethé
Laurent Fairhead
Marie‐Alice Foujols
Jean‐Yves Grandpeix
Guillaume Levavasseur
Olivier Marti
Matthew Menary
Catherine Rio
Clément Rousset
Yona Silvy
author_sort Juliette Mignot
title The Tuning Strategy of IPSL‐CM6A‐LR
title_short The Tuning Strategy of IPSL‐CM6A‐LR
title_full The Tuning Strategy of IPSL‐CM6A‐LR
title_fullStr The Tuning Strategy of IPSL‐CM6A‐LR
title_full_unstemmed The Tuning Strategy of IPSL‐CM6A‐LR
title_sort tuning strategy of ipsl‐cm6a‐lr
publisher American Geophysical Union (AGU)
publishDate 2021
url https://doaj.org/article/d0feb0d749634f6e8523a8c964ccf73c
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