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Carbon Exchange Between Atmosphere and Oceans in a Latitude-Dependent Advection-Diffusion Model

Bibliographic Data

ID9245353
AuthorsGerhard Kratz, G H Kohlmaier, E O Siré, Ursula Fischbach, Horst Bröhl
Year1983
Volume25
Issue2
Pages459-471
Publication date1983-01-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueRadiocarbon (JOURNAL)
Journal identifiersISSN: 0033-8222 • E-ISSN: 1945-5755
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s0033822200005750
OpenAlexW2489141126
LanguageEN
References cited19

Marine transport of inorganic and organic carbon is simulated by means of a computer model in which the oceans are divided into a high and low latitude region. Water transport (and with it carbon transport) is reproduced 1) as downwelling of surface waters at low latitudes, and 2) in general, as different depth-dependent turbulent diffusion in both deep-sea regions. The model is calibrated with pre-bomb 14 C and validated against perturbations of total carbon, 13 C/C- and 14 C/C-ratios; it is compatible with carbon release from fossil fuels and from biogenic sources

Advection · Atmospheric sciences · Carbon fibers · Diffusion · Downwelling · Geography · Latitude · Meteorology · Physics · Radiocarbon dating · Thermodynamics · Total organic carbon · Upwelling · Chemistry · Environmental Science · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Marine and coastal ecosystems · Materials Science · Environmental Chemistry · Geology · Oceanography · Paleontology

  • A box diffusion model to study the carbon dioxide exchange in nature

    Open Access•H Oeschger, U Siegenthaler et al.•Tellus A Dynamic Meteorology and…•1975

  • Transfer of Bomb 14 C to the Ocean Surface

    Open Access•Reidar Nydal, Knut Lövseth et al.•Radiocarbon•1980

  • Modeling the Carbon System

    Open Access•Wallace S Broecker, Tsung-Hung Peng et al.•Radiocarbon•1980

  • Allgemeine Meereskunde

    N B Marshall, Gunter Dietrich et al.•Geographical Journal•1957

Citation velocityhistorical
Highly citedNo

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