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Technical report submitted to the Department of Energy, Washington, DC on determination of net CO/sub 2/ flux across air-sea interface

Technical Report ·
OSTI ID:5914510
The net CO/sub 2/ flux across the air-sea interface has been determined in December, 1982, in the Caribbean Sea and the tropical North Atlantic Ocean using the pCO/sub 2/ and radon-222 methods. The thermodynamic driving force for CO/sub 2/ gas transfer has been characterized in terms of the difference between the CO/sub 2/ partial pressures, pCO/sub 2/, in the surface ocean water and the overlying atmosphere, and the gas exchange coefficient (expressed in terms of the piston velocity) has been estimated on the basis of the vertical distribution of radon-222 gas in the upper 200 meters of water column. The net CO/sub 2/ flux across the air-sea interface has been computed using these two quantities. The areas north of the 10/sup 0/N parallel are a CO/sub 2/ sink area, where a net CO/sub 2/ flux ranging from 0 to about 1 mole CO/sub 2//m/sup 2/ y (from air to sea) has been observed. This compares with the global mean net CO/sub 2/ flux of about 0.6 mole CO/sub 2//m/sup 2/ y (from air to sea). On the other hand, the areas south of 10/sup 0/N are a CO/sub 2/ source area. The sea-to-air net flux of as high as 3 moles CO/sub 2//m/sup 2/ y has been observed east of the mouth of the Amazon River. Although the equatorial surface water exhibited high pCO/sub 2/ values, the gas exchange piston velocity was small particularly in the doldrum, and hence the net CO/sub 2/ flux values ranging between 1 and 2 moles CO/sub 2//m/sup 2/ y were observed.
Research Organization:
Columbia Univ., Palisades, NY (USA). Lamont-Doherty Geological Observatory
DOE Contract Number:
AC02-81ER60000
OSTI ID:
5914510
Report Number(s):
DOE/ER/60000-T1; ON: DE83015577
Country of Publication:
United States
Language:
English