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    Comparing Long-Term Atmospheric 14C and 3H Records near Groningen, the Netherlands with Fruholmen, Norway and Izaña, Canary Islands 14C Stations

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    Author
    Meijer, Harro J. A.
    van der Plicht, Johannes
    Gislefoss, Jorunn S.
    Nydal, Reidar
    Issue Date
    1995-01-01
    Keywords
    Baden Wurttemberg Germany
    Atlantic Ocean Islands
    Canary Islands
    Groningen Netherlands
    Izaña
    petroleum products
    Tenerife
    hydrogen
    tritium
    Norway
    seasonal variations
    Germany
    pollution
    atmosphere
    Holocene
    Central Europe
    Netherlands
    Europe
    Western Europe
    Scandinavia
    Cenozoic
    Quaternary
    C 14
    carbon
    isotopes
    radioactive isotopes
    carbon dioxide
    geochemistry
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    Citation
    Meijer, H. J. A., van der Plicht, J., Gislefoss, J. S., & Nydal, R. (1995). Comparing long-term atmospheric 14C and 3H records near Groningen, the Netherlands with Fruholmen, Norway and Izaña, Canary Islands 14C stations. Radiocarbon, 37(1), 39-50.
    Publisher
    Department of Geosciences, The University of Arizona
    Journal
    Radiocarbon
    URI
    http://hdl.handle.net/10150/653272
    DOI
    10.1017/S0033822200014776
    Additional Links
    http://radiocarbon.webhost.uits.arizona.edu/
    Abstract
    We present the results of the 14CO2 atmospheric monitoring station at the Smilde observation station, near Groningen, the Netherlands, a typical continental station. We compared these data, for absolute values and annual variation, with data from Fruholmen, Nordkapp, Norway and Izaña, Tenerife, Canary Islands, which are situated in areas less influenced by fossil-fuel CO2. The 20-yr Smilde record shows much seasonal variation (peak-to-trough variation is approximately 30 per mil in contrast to approximately 12 per mil for Fruholmen, and approximately 5 per mil for Izaña) and a lower overall value due to fossil-fuel consumption, in accordance with findings from similar stations in continental Western Europe. The Fruholmen and Izaña data show fairly equal mean Delta-14C levels, but differ in seasonal amplitude. This difference could be due partly to the elevation difference between the stations. The Izaña station also has a slow exchange with the ground-level air because of an inversion layer. It is speculative whether annual injection of 14C from the stratosphere also plays a role. We give the Groningen long record of tritium in precipitation, showing profound seasonality.
    Type
    Article
    text
    Language
    en
    ISSN
    0033-8222
    ae974a485f413a2113503eed53cd6c53
    10.1017/S0033822200014776
    Scopus Count
    Collections
    Radiocarbon, Volume 37, Number 1 (1995)

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