Sources and flow patterns of deep-ocean waters as deduced from potential temperature, salinity, and initial phosphate concentration

Author:

Broecker Wallace S.,Takahashi Taro,Takahashi Timothy

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference32 articles.

1. GEOSECS Atlantic Expedition;Bainbridge,1981

2. On the abyssal circulation of the World Ocean, 4, Origin and rate of circulation of deep ocean water as determined with the aid of tracers;Bolin;Deep Sea Res.,1961

3. “NO” a conservative water-mass tracer;Broecker;Earth Planet. Sci. Lett.,1974

4. Is there a tie between atmospheric CO2 content and ocean circulation?;Broecker,1984

5. Broecker, W. S., , D. W., Spencer, , H., Craig, , GEOSECS Pacific Expedition: Hydrographic Data, , 3, U.S. Government Printing Office, Wash., D. C., 1982,

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