U.S.
JGOFS
Synthesis & Modeling Project |
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Kitack Lee
Collaborators:
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Degree of saturation state of CaCO3 in the oceans
NOAA/DOE OACES, 2 years |
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PROJECT DESCRIPTION: |
Over the last eight years (1990-1998) a large global database of high
quality total alkalinity (TA) and total inorganic carbon (TCO2)
measurements in the Atlantic, Pacific, and Indian Oceans has been obtained
through a multi-national and a multi-agency effort for the global CO2
surveys. The measurement campaigns included parts of the NOAA/OACES,
the DOE/WOCE, and the JGOFS CO2 survey programs. This
carbon database is unprecedented in terms of quality (2 mol kg-1in
TA and 1 mol kg-1 in TCO2) and spatial coverage.
The previous studies on the degree of saturation of CaCO3 in
the oceans (Li et al., 1969; Archer, 1996) using the historical measurements
(GEOSECS) suffered from spatially insufficient data coverage, less precise
and less accurate carbonate measurements, and inaccurate thermodynamic
constants. Therefore, it is worthwhile to revisit this issue with
recently collected global carbon data. Another interesting aspect
of this proposed research is to examine the effect of oceanic uptake of
anthropogenic CO2 on the degree of saturation state of seawater
with respect to aragonite and calcite, since the amount of anthropogenic
CO2 taken up by the oceans since the Industrial Revolution can
be detectable with presently available techniques. The rising atmospheric
CO2 concentration due to burning of fossil fuels is likely to
reduce the concentration of surface water of carbonate ion (CO32-)
by about 30% relative to the pre-industrial level as the atmospheric CO2
concentration doubles the pre-industrial level by the middle of 21st century.
A recent pioneering study (Langdon et al., 1998) suggests that changes
in the degree of saturation-state of surface seawater with respect to CaCO3
will reduce calcification rate of coral community proportionally as the
concentration of surface carbonate ion ([CO32-])
decreases. If this provocative finding can be extrapolated to all
CaCO3 bearing organisms this would mean that global production
of hard tissue would decrease with increasing pCO2, which in
turn might lead to greater oceanic uptake of CO2. Four
tangible goals below will be pursued for the execution period of this proposal:
1. Globally consistent databases for total alkalinity and total inorganic carbon;
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DATA: |
- no data submitted -
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PUBLICATIONS: |
Lee, K. 2001. Global net community production estimated from the annual cycle of surface water total dissolved inorganic carbon. Limnol. Oceanogr.
Limnology and Oceanography 46(6): 1287-1297.
Lee, K.; Millero, F.J.; Byrne, R.H.; Feely, R.A.; Wanninkhof, R. 2000. The recommended dissociation constants of carbonic acid in seawater, Geophys. Res. Lett. 27: 229-232.
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RELATED PROJECTS: |
Sabine; Key; Feely; Millero; Wanninkhof; Kozyr
"Synthesis and interpretation of the NOAA/DOE
global CO2 survey data"
Wanninhkof; Wallace; Baringer "Meridional transport of carbon dioxide in the North Atlantic Ocean"
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INVESTIGATOR
INFORMATION: |
Kitack Lee
School of Environmental Science and Engineering Pohang University of Science and Technology San 31, Hyoja-dong, Nam-gu Pohang, 790-784 Republic of Korea (formerly NOAA/AOML/OCD) tel: 82-054-279-2285 fax: 82-279-8299 ktl@postech.ac.kr http://www.aoml.noaa.gov/ocd/people/lee/ Frank J. Millero
Richard A. Feely
Rik Wanninkhof
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