Author:
Broecker W S,Peng T-H,Mathieu G,Hesslein R,Torgersen T
Abstract
Rates of CO2 exchange across the air-water interface in oceans and lakes measured to date by the L-DGO group are summarized. They range from 3 to 38 moles/m2/yr. The possible causes for this range include the differences in salinity, mean wind speed, and pH. Wind tunnel studies comparing fresh water and sea water are required before a satisfactory explanation can be found.
Publisher
Cambridge University Press (CUP)
Subject
General Earth and Planetary Sciences,Archaeology
Reference11 articles.
1. Broecker W S and Walton A , 1959, The geochemistry of C-14 in fresh-water systems: Geochim et Cosmochim Acta, v 16, p 15–38.
2. The influence of wind on CO2-exchange in a wind-wave tunnel, including the effects of monolayers;Broecker;Jour Marine Research,1978
3. Broecker W S and Peng T-H , 1971, The vertical distribution of radon in the BOMEX area: Earth Planetary Sci Letters, v 11, p 99–108.
4. Peng T-H , Broecker W S , Mathieu G G , Li T-H , and Bainbridge A E , 1979, Radon evasion rates in the Atlantic and Pacific Oceans as determined during the GEOSECS Program: Jour Geophys Research, v 84, p 2471–2486.
5. Peng T-H , Takahashi T , and Broecker W S , 1974, Surface radon measurements in the North Pacific Ocean station PAPA: Jour Geophys Research, v 79, p 1772–1780.
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