New production in the equatorial Pacific: A coupled dynamical-biogeochemical model

Fisheries Oceanography

Volumn 7, Issue 3-4, 1998, Pages 311-316

  Stoens, A ^a   Menkes, C ^a   Dandonneau, Y ^a   Memery, L ^a  

^a CNRS   (France)

Author keywords

Dissolved export production; ENSO; Equatorial Pacific; Model; New production; Salinity front

Indexed keywords

BIOGEOCHEMICAL CYCLE; BIOLOGICAL PRODUCTION; MODEL; NITRATE;

PACIFIC OCEAN;

KATSUWONUS PELAMIS;

EID: 0032419868     PISSN: 10546006     EISSN: None     Source Type: Journal    
DOI: 10.1046/j.1365-2419.1998.00079.x     Document Type: Article

References (30)

1. Archer, D., Peltzer, E.T. and Kirchman, D.L. (1997) A timescale for dissolved organic carbon production in the equatorial Pacific surface waters. Global Biogeochem. Cycl. 3:435-452.
2. Bacastow, R. and Maier-Reimer, E. (1991) Dissolved organic carbon in modeling of oceanic new production. Global Biogeochem. Cycl. 5:71-85.
3. Blanke, B. and Delecluse, P. (1993) Variability of the tropical Atlantic Ocean simulated by a general circulation model with two different mixed-layer physics. J. Phys. Oceanogr. 23:1363-1388.
4. Buesseler, K.O., Andrew, J.A., Hartman, M.C., Belastock, R. and Chai, F. (1995) Regional estimates of export flux of particulate organic carbon derived from thorium-234 during the JGOFS EqPac program. Deep-Sea Res. II 42:777-804.
5. Chai, F., Lindley, S.T. and Barber, R.T. (1996) Origin and maintenance of a high nitrate condition in the equatorial Pacific. Deep-Sea Res. II 43:1031-1064.
6. Chavez, F.P. and Barber, R.T. (1987) An estimate of new production in the equatorial Pacific. Deep-Sea Res. 34:1229-1243.
7. Chavez, F.P., Service, S.K. and Buttrey, S.E. (1996) Temperature-nitrate relationships in the central and eastern tropical Pacific. J. Geophys. Res. 101:20553-20563.
8. Dandonneau, Y. (1992) Surface chlorophyll concentration in the tropical Pacific Ocean: an analysis of data collected by merchant ships from 1978 to 1989. J. Geophys. Res. 97:3581-3591.
9. Dugdale, R.C. and Goering, J.J. (1967) Uptake of new and regenerated forms of nitrogen in primary productivity. Limnol. Oceanogr. 12:196-206.
10. Eppley, R.W. and Peterson, B.J. (1979) Particulate organic matter flux and planktonic new production in the deep ocean. Nature 282:677-680.
11. Grima, N., Bentamy, A., Delecluse, P., Katsaros, K., Levy, C. and Quilfen, Y. (1998). Sensitivity study of an Oceanic General Circulation Model forced by satellite wind-stress fields. J. Geophys. Res. (in press).
12. Honjo, S., Manganini, S.J. and Cole, J.J. (1982) Sedimentation of biogenic matter in the deep ocean. Deep-Sea Res. 29: 609-625.
13. 228Raderived nutrient budgets in the upper equatorial Pacific and the role of "new" silicate in limiting productivity. Deep-Sea Res. II 42:479-497.
14. Lehodey, P., Bertignac, M., Hampton, J., Lewis, A. and Picaut, J. (1997) El Niño Southern Oscillation and tuna in the western Pacific. Nature 389:715-717.
15. Lehodey, P., Andre, J.-M., Bertignac, M., Hampton, J., Stoens, A., Menkes, C., Mémery, L. and Grima, N. (1998) Predicting skipjack tuna forage distributions in the equatorial Pacific using a coupled dynamical bio-geochemical model. Fish. Oceanogr. 7:317-325.
16. Levitus, S., Reid, J.L., Conkright, M.E. and Najjar, R. (1983) Distribution of nitrate, phosphate and silicate in the world ocean. Progr. Oceanogr. 31:245-273.
17. Libby, P.S. and Wheeler, P.A. (1997) Particulate and dissolved organic nitrogen in the central and eastern equatorial Pacific. Deep-Sea Res. I 44:345-361.
18. 228Th: an investigation in the equatorial Pacific along 140°W. Deep-Sea Res. II 42:805-829.
19. Morel, A. (1991) Light and marine photosynthesis: a spectral model with geochemical and climatological implications. Prog. Oceanogr. 26:263-306.
20. Morel, A. and Berthon, J.F. (1989) Surface pigments, algal biomass profiles, and potential production of the euphotic layer: relationships reinvestigated in view of remote-sensing applications. Limnol. Oceanogr. 34:1545-1562.
21. Moutin, T., and Coste, B. (1996) Campagne océanografique OLIPAC à bord du N.O. l'Atalante, 3 Novembre-1 Décembre 1994, Recueil de données (Data report). Centre d'Océanologie de Marseille, 266 pp.
22. Murray, J.W., Young, J., Newton, J., Dunne, J., Chapin, T., Paul, B. and Mc Carthy, J.J. (1996) Export flux of particulate organic carbon from the central equatorial Pacific determined using a combined drifting approach. Deep-Sea Res. II 43:1095-1132.
23. Najjar, R.G., Sarmiento, J.L. and Toggweiler, J.R. (1992) Downward transport and fate of organic matter in the ocean: simulations with a general circulation model. Global Biogeochem. Cycl. 6:45-76.
24. Picaut, J., Ioualalen, M., Menkes, C., Delcroix, T. and McPhaden, M.J. (1996) Mechanism of the zonal displacements of the Pacific warm pool. Science 274:1486-1489.
25. Sarmiento, J.L., Slater, R.D., Fasham, M.J.R., Ducklow, H.W., Toggweiler, J.R. and Evans, G.T. (1993) A seasonal three-dimensional ecosystem model of nitrogen cycling in the North Atlantic euphotic zone. Global Biogeochem. Cycl. 7:417-450.
26. 2 budget. Science 247:1431-1438.
27. Toggweiler, J.R. and Carson, S. (1995) What are upwelling systems contributing to the ocean's carbon and nutrient budgets. In: Upwelling in the Ocean: Modern Processes and Ancient Records. C.P. Summerhayes, M.V. Angel, R.L. Smith and B. Zeitzschel (eds). New York: John Wiley and Sons Ltd, pp. 337-360.
28. Wyrtki, K. (1981) An estimate of equatorial upwelling in the Pacific. J. Phys. Oceanogr. 11:1205-1214.
29. Yamanaka, Y. and Tajika, E. (1997) Role of dissolved organic matter in the marine biogeochemical cycle: studies using an ocean biogeochemical general circulation model. Global Biogeochem. Cycl. 11:599-612.
30. Yoder, J.A., McClain, C.R., Feldman, G.C. and Esaias, W.E. (1993) Annual cycles of phytoplankton chlorophyll concentrations in the global ocean: a satellite view. Global Biogeochem. Cycl. 7:181-193.