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C Profiles in the Norwegian and Greenland Seas by Conventional and AMS Measurements

Bibliographic Data

ID9241669
AuthorsReidar Nydal, Jorunn Gislefoss, Ingunn Skjelvan (0000-0001-6761-5016), Fred Skogseth, A J T Jull (0000-0002-4079-4947), D J Donahue
Year1992
Volume34
Issue3
Pages717-726
Publication date1992-01-01
Open AccessYes
TypeARTICLE
VenueRadiocarbon (JOURNAL)
Journal identifiersISSN: 0033-8222 • E-ISSN: 1945-5755
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s0033822200064006
OpenAlexW2475636404
LanguageEN
Citations received4
References cited14

CO 2 in the atmosphere is an important climate gas because of its absorption of infrared radiation. More knowledge about CO 2 uptake in the ocean is of critical significance in predicting future climate development. For a period of approximately 30 years, radioactive carbon from nuclear tests has been a very useful tracer in CO 2 exchange studies. Up to now, the measurements have been based mainly on the conventional counting technique with large CO 2 samples ( ca. 5 liters). Accelerator mass spectrometry (AMS) with small CO 2 samples (1–2 ml) has made sampling much easier, and has especially stimulated the use of 14 C as a tracer in the ocean. At higher latitudes, the ocean acts as a sink for CO 2 . In addition to Δ 14 C measurements, we are concerned here with dissolved inorganic carbon (DIC) and δ 13 C in the Norwegian and Greenland Seas. During cruises in 1989 and 1990, we obtained several Δ 14 C profiles, and also repeated a few GEOSECS profiles taken in 1972. The shape of these profiles changes with time, and provides information about the mixing rate and the age of the deep water. From changes in the profiles, it appears that the deep water in the Greenland Sea has obtained about 25% of the 14 C concentration in the ocean surface over a period of 25 years. The Norwegian Sea deepwater is estimated to be 50–100 years older than that of the Greenland Sea

Accelerator mass spectrometry · Atmospheric sciences · Carbon dioxide · Dissolved organic carbon · Geography · Radiocarbon dating · Seawater · Total inorganic carbon · TRACER · Water mass · Atmospheric and Environmental Gas Dynamics · Chemistry · Environmental Science · Marine and coastal ecosystems · Methane Hydrates and Related Phenomena · Geology · Oceanography

  • Reidar Nydal (1926–2004)

    Open Access•Marian Scott, E Marian Scott•Radiocarbon•2004

  • Preparation of Graphite Targets from Small Marine Samples for AMS Radiocarbon Measurements

    Open Access•Laval Liong Wee Kwong, Pavel P Povinec et al.•Radiocarbon•2004

  • Status report of the Trondheim Radiocarbon Laboratory

    Open Access•Martin Seiler, Pieter M Grootes et al.•Radiocarbon•2019

  • Further Application of Bomb 14 C as a Tracer in the Atmosphere and Ocean

    Open Access•Reidar Nydal, Jorunn S Gislefoss•Radiocarbon•1996

  • Tracing bomb 14 C in the atmosphere 1962–1980

    Open Access•Reidar Nydal, Knut Lövseth•Journal of Geophysical Research:…•1983

  • An Analysis of Shielding Efficiency for 14 C Counters

    Open Access•Reidar Nydal, Steinar Gulliksen et al.•Radiocarbon•1980

  • Operation of the NSF-Arizona Accelerator Facility for Radioisotope Analysis and Results from Selected Collaborative Research Projects

    Open Access•T W Linick, A J T Jull et al.•Radiocarbon•1986

  • Radiocarbon in Dissolved Organic and Inorganic Carbon From the Central North Pacific

    Ellen R M Druffel, Peter M Williams et al.•Radiocarbon•1989

  • Discussion Reporting of 14 C Data

    Open Access•Minze Stuiver, Henry A Polach•Radiocarbon•1977

  • Bomb 14 C in the Ocean Surface 1966–1981

    Open Access•Reidar Nydal, Steinar Gulliksen et al.•Radiocarbon•1984

Citations per year0.13
Citation span1996 - 2019 (24)
Highly citedNo

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