Hostname: page-component-586b7cd67f-t8hqh Total loading time: 0 Render date: 2024-11-25T08:38:17.209Z Has data issue: false hasContentIssue false
  • English
  • Français

Comparing Long-Term Atmospheric 14C and 3H Records Near Groningen, the Netherlands with Fruholmen, Norway and Izaña, Canary Islands 14C Stations1

Published online by Cambridge University Press:  18 July 2016

Harro A. J. Meijer ,
Johannes van der Plicht ,
Jorunn S. Gislefoss  and
Reidar Nydal
Harro A. J. Meijer
Affiliation:
Centrum voor Isotopen Onderzoek, University of Groningen, NL-9747 AG Groningen The Netherlands
Johannes van der Plicht
Affiliation:
Centrum voor Isotopen Onderzoek, University of Groningen, NL-9747 AG Groningen The Netherlands
Jorunn S. Gislefoss
Affiliation:
Radiological Dating Laboratory, NTH, N-7034 Trondheim, Norway
Reidar Nydal
Affiliation:
Radiological Dating Laboratory, NTH, N-7034 Trondheim, Norway
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

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 ∼30‰ in contrast to ∼12‰ for Fruholmen, and ∼5‰ 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 Δ14C 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
Articles
Information
Radiocarbon , Volume 37 , Issue 1 , 1995 , pp. 39 - 50
Copyright
Copyright © The American Journal of Science 

References

Broecker, W. S., Peng, T. H., Östlund, G. and Stuiver, M. 1985 The distribution of bomb radiocarbon in the ocean. Journal of Geophysical Research 90(C4): 6953–6970.Google Scholar
CDIAC (Carbon Dioxide Information Analysis Center) database, Oak Ridge, Tennessee, Oak Ridge National Laboratory. Internet URL: http://cdiac.esd.ornl.gov/cdiac/.Google Scholar
Cleveland, W. S., and McRae, J. E. 1989 The use of loess and STL in the analysis of atmospheric CO2 and related data. in Elliot, W. P., ed., The Statistical Treatment of CO2 Data Records. Silver Spring, Maryland, NOAA Tech memo ERL ARL-173.Google Scholar
Gislefoss, J. S. 1994. (ms.) Carbon Profiles in the Nordic Seas. Ph.D. dissertation, Radiological Dating Laboratory, UNIT/NTH, Trondheim, Norway.Google Scholar
IAEA 1979 Behaviour of Tritium in the Environment, Proceedings of an International Symposium on the Behaviour of Tritium, San Francisco 1978. Vienna, IAEA proceedings series 498.Google Scholar
IAEA 1994 Environmental Isotope Data No. 10. Vienna, IAEA Technical Reports series no. 371.Google Scholar
Hesshaimer, V., Heimann, M. and Levin, I. 1994 Radiocarbon evidence for a smaller oceanic carbon dioxide sink than previously believed. Nature 370: 201–203.Google Scholar
Levin, I., Graul, R. and Trivett, N. B. A. 1995 Long term observations of atmospheric CO2 and carbon isotopes at continental sites in Germany. Tellus 47B(1/2): 23–24.CrossRefGoogle Scholar
Levin, I., Münnich, K. O., and Weiss, W. 1980 The effect of anthropogenic CO2 and 14C sources on the distribution of 14C in the atmosphere. in Stuiver, M. and Kra, R. S., eds, Proceedings of the 10th International 14C conference. Radiocarbon 22(2): 379–391.Google Scholar
Levin, I., Schuchard, J., Kromer, B., and Münnich, K. O. 1989 The continental European Suess effect. in Long, A. and Kra, R. S., eds, Proceedings of the 13th International 14C conference. Radiocarbon 31(3): 431–440.Google Scholar
Manning, M. R., Lowe, D. C., Melhuish, W. H., Sparks, R. J., Wallace, G., Brenninkmeijer, C. A. M. and McGill, R. C. 1990 The use of radiocarbon measurements in atmospheric studies. Radiocarbon 32(1): 37–58.Google Scholar
Münnich, K. O. and Vogel, J. C. 1958 Durch Atomexplosionen erzeugter Radiokohlenstoff in der Atmosphäre. Naturwissenschaften 45: 327–329.CrossRefGoogle Scholar
Nydal, R. 1966 Variation in 14C concentration in the atmosphere during the last several years. Tellus 18(2): 271–279.Google Scholar
Nydal, R. 1968 Further investigation of the transfer of radiocarbon in nature. Journal of Geophysical Research 73: 3617–3634.CrossRefGoogle Scholar
Nydal, R. 1991. Exchange of CO2 between the atmosphere and the ocean. Norsk Geologisk Tidsskrift 71: 199–201.Google Scholar
Nydal, R., Gulliksen, S., Lövseth, K. and Skogseth, F. H. 1984 Bomb 14C in the ocean surface 1966-1981. Radiocarbon 26(1): 7–45.Google Scholar
Nydal, R. and Lövseth, K. 1983 Tracing Bomb 14C in the atmosphere 1962-1980. Journal of Geophysical Research 88: 3621–3642.Google Scholar
Schlesinger, W.H. 1991 Biogeochemistry: An Analysis of Global Change. San Diego, California, Academic Press: 443 P.Google Scholar
Stuiver, M. and Polach, H. A. 1977 Discussion: Reporting of 14C data. Radiocarbon 19(3): 355–363.Google Scholar
Tans, P. P. 1978 (ms.) Carbon 13 and Carbon 14 in Trees and the Atmospheric CO2 increase. Ph.D. Dissertation, University of Groningen.Google Scholar
Vogel, J. C. 1970 Groningen radiocarbon dates IX. Radiocarbon 12(2): 444–471.Google Scholar
Zondervan, A, and Meijer, H. A. J. 1995 The start of an “event trapping” air monitoring station at Kollumerwaard, NL. in Rozanski, K., ed., Isotope Variations of Carbon Dioxide and other Trace Gases in the Atmosphere. Final Report of the Final Research Coordinating Meeting, Vienna, November 7-10, 1994. Vienna, Austria, IAEA.Google Scholar