Evaluating global ocean carbon models: The importance of realistic physics
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The formation of the ocean's anthropogenic carbon reservoirEcosystem dynamics based on plankton functional types for global ocean biogeochemistry modelsBiological responses to environmental heterogeneity under future ocean conditions.Localized subduction of anthropogenic carbon dioxide in the Southern Hemisphere oceansOceanic sources, sinks, and transport of atmospheric CO2Nitrogen fixation amplifies the ocean biogeochemical response to decadal timescale variations in mineral dust depositionVariational data assimilation for atmospheric CO2Model uncertainty in the ecosystem approach to fisheriesContribution of ocean, fossil fuel, land biosphere, and biomass burning carbon fluxes to seasonal and interannual variability in atmospheric CO2Assessing the magnitude of CO2flux uncertainty in atmospheric CO2records using products from NASA's Carbon Monitoring Flux Pilot ProjectImpact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)Denitrification under glacial and interglacial conditions: A physical approachDecadal biogeochemical changes in the subtropical Indian Ocean associated with Subantarctic Mode WaterSkill assessment of three earth system models with common marine biogeochemistryQuantitative interpretation of atmospheric carbon records over the last glacial terminationInverse estimates of the oceanic sources and sinks of natural CO2 and the implied oceanic carbon transportInverse estimates of anthropogenic CO2uptake, transport, and storage by the oceanExplicit Planktic Calcifiers in the University of Victoria Earth System Climate Model, Version 2.9Nitrogen isotope simulations show the importance of atmospheric iron deposition for nitrogen fixation across the Pacific OceanUsing tracer observations to reduce the uncertainty of ocean diapycnal mixing and climate-carbon cycle projectionsAdiabatic reduction of circulation-related CO2air-sea flux biases in a North Atlantic carbon-cycle modelRapid decline of the CO2buffering capacity in the North Sea and implications for the North Atlantic OceanCauses and implications of persistent atmospheric carbon dioxide biases in Earth System ModelsParticle flux in the oceans: Challenging the steady state assumptionImpacts of increasing anthropogenic soluble iron and nitrogen deposition on ocean biogeochemistryChanging controls on oceanic radiocarbon: New insights on shallow-to-deep ocean exchange and anthropogenic CO2uptakeOceanic ventilation and biogeochemical cycling: Understanding the physical mechanisms that produce realistic distributions of tracers and productivityFraming biological responses to a changing oceanAir-sea disequilibrium of carbon dioxide enhances the biological carbon sequestration in the Southern OceanRole of the Southern Annular Mode (SAM) in Southern Ocean CO2uptake
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Evaluating global ocean carbon models: The importance of realistic physics
description
article
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wetenschappelijk artikel
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наукова стаття, опублікована у вересні 2004
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name
Evaluating global ocean carbon models: The importance of realistic physics
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Evaluating global ocean carbon models: The importance of realistic physics
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type
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Evaluating global ocean carbon models: The importance of realistic physics
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Evaluating global ocean carbon models: The importance of realistic physics
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prefLabel
Evaluating global ocean carbon models: The importance of realistic physics
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Evaluating global ocean carbon models: The importance of realistic physics
@nl
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P2860
P50
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P1476
Evaluating global ocean carbon models: The importance of realistic physics
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E. Maier-Reimer
G.-K. Plattner
I. J. Totterdell
J. C. Marshall
J. Sarmiento
J.-C. Dutay
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10.1029/2003GB002150
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P577
2004-09-01T00:00:00Z