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Title: CO/sub 2/ fluxes in the tropical Atlantic during FOCAL cruises

Journal Article · · J. Geophys. Res.; (United States)
OSTI ID:6085685

CO/sub 2/ partial pressures in the atmosphere and in surface seawater have been measured in the equatorial Atlantic Ocean during Programme Francais Ocean-Climat en Atlantique Equatorial cruises extending from July 1982 to August 1984 along the 4/degree/W, 22/degree/W, and 35/degree/W meridians. Gas transfer coefficients based on recently reported field data combined with information deduced from wind tunnel experiments are used to compute the CO/sub 2/ fluxes. The global mean net flux between 5/degree/N and 5/degree/S is equal to 1.05 mmol m/sup /minus/2/ d/sup /minus/1/ and is from the ocean to the atmosphere. The escape of CO/sub 2/ increases strongly from the east to the west and is always lower in the north than in the south. The importance of wind speed, pCO/sub 2/ in atmosphere, PCO/sub 2/ in surface seawater, and temperature on the flux variability is discussed. The relative influence of the equatorial upwelling on one hand and of the advection and warming of surface waters on the other hand is studied in order to explain high partial pressure in seawater. 59 refs., 15 figs., 5 tabs.

Research Organization:
Laboratoire d'Oceanographie Dynamique et de Climatologie, Departement de Physico-Chimie, Gif-sur-Yvette, France; Office de la Recherche Scientifique et Technique d'Outre-Mer, Dakar, Senegal
OSTI ID:
6085685
Journal Information:
J. Geophys. Res.; (United States), Vol. 91:C10
Country of Publication:
United States
Language:
English