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dc.contributor.authorJiang, Li-Qing
dc.contributor.authorDunne, John
dc.contributor.authorCarter, Brendan R
dc.contributor.authorTjiputra, Jerry
dc.contributor.authorTerhaar, Jens
dc.contributor.authorSharp, Jonathan D.
dc.contributor.authorOlsen, Are
dc.contributor.authorAlin, Simone
dc.contributor.authorBakker, Dorothee C.E.
dc.contributor.authorFeely, Richard A.
dc.contributor.authorGattuso, Jean-Pierre
dc.contributor.authorHogan, Patrick
dc.contributor.authorIlyina, Tatiana
dc.contributor.authorLange, Nico
dc.contributor.authorLauvset, Siv Kari
dc.contributor.authorLewis, Ernie R.
dc.contributor.authorLovato, Tomas
dc.contributor.authorPalmieri, Julien
dc.contributor.authorSantana-Falcòn, Yeray
dc.contributor.authorSchwinger, Jörg
dc.contributor.authorSéférian, Roland
dc.contributor.authorStrand, Gary
dc.contributor.authorSwart, Neil
dc.contributor.authorTanhua, Toste
dc.contributor.authorTsujino, Hiroyuki
dc.contributor.authorWanninkhof, Rik
dc.contributor.authorWatanabe, Michio
dc.contributor.authorYamamoto, Akitomo
dc.contributor.authorZiehn, Tilo
dc.date.accessioned2023-08-15T12:12:22Z
dc.date.available2023-08-15T12:12:22Z
dc.date.created2023-05-03T17:08:48Z
dc.date.issued2023
dc.identifier.issn1942-2466
dc.identifier.urihttps://hdl.handle.net/11250/3084154
dc.description.abstractAccurately predicting future ocean acidification (OA) conditions is crucial for advancing OA research at regional and global scales, and guiding society's mitigation and adaptation efforts. This study presents a new model-data fusion product covering 10 global surface OA indicators based on 14 Earth System Models (ESMs) from the Coupled Model Intercomparison Project Phase 6 (CMIP6), along with three recent observational ocean carbon data products. The indicators include fugacity of carbon dioxide, pH on total scale, total hydrogen ion content, free hydrogen ion content, carbonate ion content, aragonite saturation state, calcite saturation state, Revelle Factor, total dissolved inorganic carbon content, and total alkalinity content. The evolution of these OA indicators is presented on a global surface ocean 1° × 1° grid as decadal averages every 10 years from preindustrial conditions (1750), through historical conditions (1850–2010), and to five future Shared Socioeconomic Pathways (2020–2100): SSP1-1.9, SSP1-2.6, SSP2-4.5, SSP3-7.0, and SSP5-8.5. These OA trajectories represent an improvement over previous OA data products with respect to data quantity, spatial and temporal coverage, diversity of the underlying data and model simulations, and the provided SSPs. The generated data product offers a state-of-the-art research and management tool for the 21st century under the combined stressors of global climate change and ocean acidification. The gridded data product is available in NetCDF at the National Oceanic and Atmospheric Administration (NOAA) National Centers for Environmental Information: https://www.ncei.noaa.gov/data/oceans/ncei/ocads/metadata/0259391.html, and global maps of these indicators are available in jpeg at: https://www.ncei.noaa.gov/access/ocean-carbon-acidification-data-system/synthesis/surface-oa-indicators.html.en_US
dc.language.isoengen_US
dc.publisherAGUen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleGlobal Surface Ocean Acidification Indicators From 1750 to 2100en_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2023 The Author(s)en_US
dc.source.articlenumbere2022MS003563en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.doi10.1029/2022MS003563
dc.identifier.cristin2145253
dc.source.journalJournal of Advances in Modeling Earth Systemsen_US
dc.relation.projectNorges forskningsråd: 275268en_US
dc.relation.projectNorges forskningsråd: 270061en_US
dc.relation.projectSigma2: 2345en_US
dc.relation.projectSigma2: 9560en_US
dc.relation.projectSigma2: 1002en_US
dc.identifier.citationJournal of Advances in Modeling Earth Systems. 2023, 15 (3), e2022MS003563.en_US
dc.source.volume15en_US
dc.source.issue3en_US


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