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dc.contributor.authorJones, Steve D.
dc.contributor.authorLe Quéré, Corinne
dc.contributor.authorRödenbeck, Christian
dc.contributor.authorManning, Andrew C.
dc.contributor.authorOlsen, Are
dc.date.accessioned2016-05-26T09:48:24Z
dc.date.available2016-05-26T09:48:24Z
dc.date.issued2015-10-24
dc.PublishedJournal of Advances in Modeling Earth Systems 2015, 7(4):1554-15575eng
dc.identifier.issn1942-2466en_US
dc.identifier.urihttps://hdl.handle.net/1956/12015
dc.description.abstractWe have developed a statistical gap-filling method adapted to the specific coverage and properties of observed fugacity of surface ocean CO2 (fCO2). We have used this method to interpolate the Surface Ocean CO2 Atlas (SOCAT) v2 database on a 2.5°×2.5° global grid (south of 70°N) for 1985–2011 at monthly resolution. The method combines a spatial interpolation based on a “radius of influence” to determine nearby similar fCO2 values with temporal harmonic and cubic spline curve-fitting, and also fits long-term trends and seasonal cycles. Interannual variability is established using deviations of observations from the fitted trends and seasonal cycles. An uncertainty is computed for all interpolated values based on the spatial and temporal range of the interpolation. Tests of the method using model data show that it performs as well as or better than previous regional interpolation methods, but in addition it provides a near-global and interannual coverage.en_US
dc.language.isoengeng
dc.publisherAGU Publicationsen_US
dc.rightsAttribution CC BY 4.0eng
dc.rights.urihttp://creativecommons.org/licenses/by/4.0eng
dc.subjectoceaneng
dc.subjectinterpolationeng
dc.subjectCO2eng
dc.titleA statistical gap-filling method to interpolate global monthly surface ocean carbon dioxide dataen_US
dc.typePeer reviewed
dc.typeJournal article
dc.date.updated2016-03-08T10:46:04Z
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2015 The Authorsen_US
dc.identifier.doihttps://doi.org/10.1002/2014ms000416
dc.identifier.cristin1336958
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400en_US


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Attribution CC BY 4.0
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