Geoscience Reference
In-Depth Information
Le Quéré, C., Raupach, M.R., Canadell, J.G.
et al.
(2009).
Trends in the sources and sinks of carbon dioxide.
Nature
Geoscience
,
2
, 831-6.
Louanchi, F., Boudjakdji, M., and Nacef, L. (2009). Decadal
changes in surface carbon dioxide and related variables
in the Mediterranean Sea as inferred from a coupled
data-diagnostic model approach.
ICES Journal of Marine
Science
,
66
, 1538-46.
McNeil, B. and Matear, R. (2006). Projected climate change
impact on oceanic acidii cation.
Carbon Balance and
Management
,
1
, 10.1186/1750-0680-1-2
McNeil, B. and Matear, R. (2008). Southern Ocean acidii -
cation: a tipping point at 450-ppm atmospheric CO
2
.
Proceedings of the National Academy of Sciences USA
,
105
,
18860-4.
Maier, C, Hegeman, J., Weinbauer, M.G., and Gattuso, J.-P.
(2009). Calcii cation of the cold-water coral
Lophelia per-
tusa
under ambient and reduced pH.
Biogeosciences
,
6
,
1671-80.
Matsumoto, K., Sarmiento, J.L., Key, R.M.
et al.
(2004).
Evaluation of ocean carbon cycle models with data-
based metrics.
Geophysical Research Letters
,
31
, L07303,
doi:10.1029/2003GL018970.
Meehl, G.A., Stocker, T.F., Collins, W.D.
et al.
(2007). Global
climate projections. In: S. Solomon, D. Qin, M. Manning
et al.
(eds),
Climate change 2007: the physical science basis.
Contribution of Working Group I to the Fourth Assessment
Report of the Intergovernmental Panel on Climate Change,
pp. 747-845. Cambridge University Press, Cambridge.
Merico, A., Tyrrell, T., and Cokacar, T. (2006). Is there any
relationship between phytoplankton seasonal dynamics
and the carbonate system?
Journal of Marine Systems
,
59
,
120-42.
Najjar, R.G., Jin, X., Louanchi, F.
et al.
(2007). Impact of cir-
culation on export production, dissolved organic mat-
ter, and dissolved oxygen in the ocean: results from
phase II of the Ocean Carbon-cycle Model
Intercomparison Project (OCMIP-2).
Global Biogeo-
chemical Cycles
,
21
, GB3007, doi:10.1029/2006GB002857.
Naki
three-dimensional
global
ocean
models.
Global
Biogeochemical Cycles
,
15
, 43-60.
Orr, J.C., Fabry, V.J., Aumont, O.
et al.
(2005) Anthropogenic
ocean acidii cation over the twenty-i rst century and its
impact on calcifying organisms.
Nature,
437
, 681-6.
Pytkowicz, R.M. and Small, L.F. (1977). Fossil fuel prob-
lem and carbon dioxide: an overview. In: N. Anderson
and A. Malahoff, A. (eds),
The fate of fossil fuel CO
2
in the
oceans
, pp. 7-29, Plenum, New York.
Revelle, R. and Suess, H.E. (1957). Carbon dioxide
exchange between atmosphere and ocean and the ques-
tion of an increase of atmospheric CO
2
during past dec-
ades.
Tellus
,
9
, 18-27.
Sabine, C.L., Feely, R.A., Gruber, N.
et al.
(2004). The oce-
anic sink for anthropogenic CO
2
.
Science
,
305
, 367-71.
Salisbury, J., Green, M., Hunt, C., and Campbell, J. (2008).
Coastal acidii cation by rivers: a new threat to shelli sh?
EOS Transactions, American Geophysical Union
,
89
, 513.
Santana-Casiano, J. M., González-Dávila, M., Rueda, M.-J.,
Llinás, O., and González-Dávila, E.-F. (2007). The
interannual variability of oceanic CO
2
parameters in
the northeast Atlantic subtropical gyre at the ESTOC
site.
Global Biogeochemical Cycles
,
21
, GB1015, doi:
10.1029/2006GB002788.
Sarmiento, J.L. and Gruber, N. (2006).
Ocean biogeochemi-
cal dynamics
, 503 pp. Princeton University Press,
Princeton, NJ.
Sarmiento, J.L., Orr, J.C., and Siegenthaler, U. (1992). A
perturbation simulation of CO
2
uptake in an ocean gen-
eral circulation model.
Journal of Geophysical Research
,
97
,
3621-45.
Sarmiento, J.L., Le Quéré, C., and Pacala, S. (1995). Limiting
future atmospheric carbon dioxide.
Global Biogeochemical
Cycles
,
9
, 121-37.
Sarmiento, J., Monfray, P., Maier-Reimer, E., Aumont, O.,
Murnane, R., and Orr, J.C. (2000). Sea-air CO
2
l uxes
and carbon transport: a comparison of three ocean gen-
eral circulation models.
Global Biogeochemical Cycles
,
14
,
1267-81.
Skirrow, G. and Whiti eld M. (1975). The effect of increases
in the atmospheric carbon dioxide content on the car-
bonate ion concentration of surface ocean water at 25°C.
Limnology and Oceanography
,
20
, 103-8.
Steinacher, M., Joos, F., Frölicher, T.L., Plattner, G.-K., and
Doney, S.C. (2009). Imminent ocean acidii cation in the
Arctic projected with the NCAR global coupled carbon
cycle-climate model.
Biogeosciences
,
6
, 515-33.
Stumm, W. and Morgan, J.J. (1970).
Aquatic chemistry
, 583
pp. Wiley, New York.
Sundquist, E.T., Plummer, L.N., and Wigley, T.M.L. (1979).
Carbon dioxide in the ocean surface: the homogeneous
buffer factor.
Science
,
204
, 1203-5.
, N. and Swart, R. (2000).
Special report on emis-
sions scenarios
, 598 pp. Intergovernmental Panel on Climate
Change, Cambridge University Press, Cambridge.
Olafsson, J., Olafsdottir, S.R., Benoit-Cattin, A., Danielsen,
M., Arnarson, T.S., and Takahashi, T. (2009). Rate of
Iceland Sea acidii cation from time series measure-
ments.
Biogeosciences
,
6
, 2661-8.
Omta, A.W., Goodwin, P., and Follows, M.J. (2010), Multiple
regimes of air-sea carbon partitioning identii ed from
constant-alkalinity buffer factors.
Global Biogeochemical
Cycles,
24
, GB3008, doi:10.1029/2009GB003726.
Orr, J.C., Maier-Reimer, E., Mikolajewicz, U.
et al.
(2001).
Estimates of anthropogenic carbon uptake for four
ć
enovi
ć