Evaluation de la pénétration du carbone anthropique en Méditerranée | Bibliographie
148
BOULAHDID, M., MINSTER, J.F., 1989. Oxygen consumption and nutrient regeneration
ratios along isopycnal horizons in the Pacific Ocean. Mar. Chem., 26, 133–153.
https://doi.org/10.1016/0304-4203(89)90057-1
BOUZINAC, C., VAZQUEZ, J., FONT, J., 1998. Complex empirical orthogonal functions
analysis of ERS-1 and TOPEX/POSEIDON combined altimetric data in the region of
the Algerian current. J. Geophys. Res. Oceans, 103, 8059–8071.
https://doi.org/10.1029/97JC02909
BREWER, P.G., 1978. Direct observation of the oceanic CO2 increase. Geophys. Res. Lett.,
997–1000.
https://doi.org/10.1029/GL005i012p00997@10.1002/(ISSN)19448007.GRL40
BRLi, 2014. Étude de la gestion quantitative du fleuve Rhône à l’étiage : Principaux résultats.
l’Agence de l’eau Rhône Méditerranée Corse et la DREAL délégation de bassin, France.
BROECKER, W.S., PENG, T., 1982. Tracers in the sea, Lamont-Doherty Geological
Observatory, Columbia University. ed. New York: 714 p.
BROECKER, W.S., PENG, T.-H., 1989. The cause of the glacial to interglacial atmospheric
CO2 change: A Polar Alkalinity Hypothesis. Glob. Biogeochem. Cycles, 3, 215–239.
https://doi.org/10.1029/GB003i003p00215
BROECKER, W.S., TAKAHASHI, TARO, TAKAHASHI, TIMOTHY, 1985. Sources and
flow patterns of deep-ocean waters as deduced from potential temperature, salinity, and
initial phosphate concentration. J. Geophys. Res. Oceans, 90, 6925–6939.
https://doi.org/10.1029/JC090iC04p06925
BRYDEN, H.L., 2003. Changes in Ocean Water Mass Properties: Oscillations or Trends?
Science, 300, 2086–2088. https://doi.org/10.1126/science.1083980
CALDEIRA, K., WICKETT, M.E., 2003. Anthropogenic carbon and ocean pH. Nature, 425,
365–365. https://doi.org/10.1038/425365a
CANALS, M., PUIG, P., MADRON, X.D. DE, HEUSSNER, S., PALANQUES, A., FABRES,
J.,
2006.
Flushing
submarine
canyons.
Nature,
444,
354–357.
https://doi.org/10.1038/nature05271
CANDELA, J., 2001. Mediterranean water and global circulation, in: Ocean Circulation and
Climate: Observing and Modelling the Global Ocean, International Geophysics Series,
77. pp. 419–429.
CDIAC, 2010. Carbon Dioxide Information Analysis Center [WWW Document]. URL
https://cdiac.ess-dive.lbl.gov/# (accessed 3.28.20).
CHAPMAN, R., NOF, D., 1988. The Sinking of Warm-Core Rings. J. Phys. Oceanogr., 18,
565–583. https://doi.org/10.1175/1520-0485(1988)018<0565:TSOWCR>2.0.CO;2
CHEN, C.-T.A., 1993a. Carbonate chemistry of the wintertime Bering Sea marginal ice zone.
Cont. Shelf Res., 13, 67–87. https://doi.org/10.1016/0278-4343(93)90036-W
CHEN, C.-T.A., 1993b. The oceanic anthropogenic CO2 sink. Chemosphere, 27, 1041–1064.
https://doi.org/10.1016/0045-6535(93)90067-F
CHEN, C.-T.A., ANDREEV, A., KIM, K.-R., YAMAMOTO, M., 2004. Roles of Continental
Shelves and Marginal Seas in the Biogeochemical Cycles of the North Pacific Ocean.
J. Oceanogr., 60, 17–44. https://doi.org/10.1023/B:JOCE.0000038316.56018.d4
CHEN, C.-T.A., HOU, W.-P., GAMO, T., WANG, S.L., 2006a. Carbonate-related parameters
of subsurface waters in the West Philippine, South China and Sulu Seas. Mar. Chem.,
99, 151–161. https://doi.org/10.1016/j.marchem.2005.05.008
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