Transfer of Bomb 14 C to the Ocean Surface

  • Nydal R
  • Lövseth K
  • Skogseth F
N/ACitations
Citations of this article
7Readers
Mendeley users who have this article in their library.

Abstract

Additional 14 C data from the atmosphere and ocean have been provided since the ninth 14 C conference in 1976. At the moment, one sampling station in the troposphere in each hemisphere seems to give sufficient accuracy for exchange studies. The 14 C concentration in the troposphere in December 1978 constituted a mean value of 30 ± 1 percent (Δ 14 C) above normal level, a concentration that has been reduced to about one half during 12 years. 14 C measurements have been performed with intervals of 1 to 4 months in the surface water of the Atlantic, Pacific, and Indian Oceans. In addition to the 14 C data observed, the salinity and temperature are also measured. Because of earlier objections against storing sea water in steel drums on board ships for months before treatment, the CO 2 has now been flushed out immediately after collection. The reliability of previous measurements has been confirmed with 10 parallel samples. 14 C concentration in ocean surface on each location shows some seasonal variation due to variable exchange of water with deeper layers.

Cite

CITATION STYLE

APA

Nydal, R., Lövseth, K., & Skogseth, F. H. (1980). Transfer of Bomb 14 C to the Ocean Surface. Radiocarbon, 22(3), 626–635. https://doi.org/10.1017/s0033822200009991

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free