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Biogeochemical protocols and diagnostics for the CMIP6 Ocean Model Intercomparison Project (OMIP)

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BORIS DOI
10.7892/boris.101617
Date of Publication
2017
Publication Type
Article
Division/Institute

Oeschger Centre for C...

Author
Orr, James C.
Najjar, Raymond G.
Aumont, Olivier
Bopp, Laurent
Bullister, John L.
Danabasoglu, Gokhan
Doney, Scott C.
Dunne, John P.
Dutay, Jean-Claude
Graven, Heather
Griffies, Stephen M.
John, Jasmin G.
Joos, Fortunatorcid-logo
Oeschger Centre for Climate Change Research (OCCR)
Physikalisches Institut, Klima- und Umweltphysik (KUP)
Levin, Ingeborg
Lindsay, Keith
Matear, Richard J.
McKinley, Galen A.
Mouchet, Anne
Oschlies, Andreas
Romanou, Anastasia
Schlitzer, Reiner
Tagliabue, Alessandro
Tanhua, Toste
Yool, Andrew
Subject(s)

500 - Science::530 - ...

500 - Science::550 - ...

Series
Geoscientific model development (GMD)
ISSN or ISBN (if monograph)
1991-959X
Publisher
Copernicus Publications
Language
English
Publisher DOI
10.5194/gmd-10-2169-2017
Description
The Ocean Model Intercomparison Project (OMIP) focuses on the physics and biogeochemistry of the ocean component of Earth system models participating in the sixth phase of the Coupled Model Intercomparison Project (CMIP6). OMIP aims to provide standard protocols and diagnostics for ocean models, while offering a forum to promote their common assessment and improvement. It also offers to compare solutions of the same ocean models when forced with reanalysis data (OMIP simulations) vs. when integrated within fully coupled Earth system models (CMIP6). Here we detail simulation protocols and diagnostics for OMIP's biogeochemical and inert chemical tracers. These passive-tracer simulations will be coupled to ocean circulation models, initialized with observational data or output from a model spin-up, and forced by repeating the 1948–2009 surface fluxes of heat, fresh water, and momentum. These so-called OMIP-BGC simulations include three inert chemical tracers (CFC-11, CFC-12, SF₆) and biogeochemical tracers (e.g., dissolved inorganic carbon, carbon isotopes, alkalinity, nutrients, and oxygen). Modelers will use their preferred prognostic BGC model but should follow common guidelines for gas exchange and carbonate chemistry. Simulations include both natural and total carbon tracers. The required forced simulation (omip1) will be initialized with gridded observational climatologies. An optional forced simulation (omip1-spunup) will be initialized instead with BGC fields from a long model spin-up, preferably for 2000 years or more, and forced by repeating the same 62-year meteorological forcing. That optional run will also include abiotic tracers of total dissolved inorganic carbon and radiocarbon, CTabio and ¹⁴CTabio, to assess deep-ocean ventilation and distinguish the role of physics vs. biology. These simulations will be forced by observed atmospheric histories of the three inert gases and CO₂ as well as carbon isotope ratios of CO₂. OMIP-BGC simulation protocols are founded on those from previous phases of the Ocean Carbon-Cycle Model Intercomparison Project. They have been merged and updated to reflect improvements concerning gas exchange, carbonate chemistry, and new data for initial conditions and atmospheric gas histories. Code is provided to facilitate their implementation.
Related URL
http://www.geosci-model-dev.net/10/2169/2017/gmd-10-2169-2017-assets.html
Handle
https://boris-portal.unibe.ch/handle/20.500.12422/153483
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File(s)
FileFile TypeFormatSizeLicensePublisher/Copright statementContent
gmd-10-2169-2017.pdftextAdobe PDF1.45 MBpublishedOpen
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