Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Carbon dioxide transport by ocean currents at 25 degrees N Latitude in the Atlantic Ocean

Journal Article · · Science (Washington, D.C.); (USA)
;  [1];  [2]
  1. Woods Hole Oceanographic Institution, MA (USA)
  2. Chalmers Univ. of Technology, Goeteborg (Sweden)
Measured concentrations of CO{sub 2}, O{sub 2}, and related chemical species in a section across the Florida Straits and in the open Atlantic Ocean at approximately 25{degrees}N, have been combined with estimates of oceanic mass transport to estimate both the gross transport of CO{sub 2} by the ocean at this latitude and the net CO{sub 2} flux from exchange with the atmosphere. The northward flux was 63.9 {times} 10{sup 6} moles per second (mol/s); the southward flux was 64.6 {times} 10{sup 6} mol/s. These values yield a net CO{sub 2} flux of 0.7 {times} 10{sup 6} mol/s (0.26 {plus minus} 0.03 gigaton of C per year) southward. The North Atlantic Ocean has been considered to be a strong sink for atmospheric CO{sub 2}, yet these results show that the net flux in 1988 across 25{degrees}N was small. For O{sub 2} the equivalent signal is 4.89 {times} 10{sup 6} mol/s northward and 6.97 {times} 10{sup 6} mol/s southward, and the net transport is 2.08 {times} 10{sup 6} mol/s or three times the net CO{sub 2} flux. These data suggest that the North Atlantic Ocean is today a relatively small sink for atmospheric CO{sub 2}, in spite of its large heat loss, but a larger sink for O{sub 2} because of the additive effects of chemical and thermal pumping on the CO{sub 2} cycle but their near equal and opposite effects on the CO{sub 2} cycle.
OSTI ID:
6536639
Journal Information:
Science (Washington, D.C.); (USA), Journal Name: Science (Washington, D.C.); (USA) Vol. 246:4929; ISSN SCIEA; ISSN 0036-8075
Country of Publication:
United States
Language:
English