Model-based evaluation of methods to determine C:N and N:P regeneration ratios from dissolved nutrients

Global Biogeochemical Cycles

Volumn 19, Issue 2, 2005, Pages 1-18

  Schneider, Birgit ^a,b   Karstensen, Johannes ^a   Oschlies, Andreas ^a,c   Schlitzer, Reiner ^d  

^a GEOMAR HELMHOLTZ CENTRE FOR OCEAN RESEARCH KIEL   (Germany)

^b UNIVERSITY OF KIEL   (Germany)

^c NATIONAL OCEANOGRAPHY CENTRE   (United Kingdom)

^d ALFRED WEGENER INSTITUTE FOR POLAR AND MARINE RESEARCH   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

BIOGEOCHEMICAL CYCLE; ORGANIC MATTER; REMINERALIZATION;

EID: 27644501131     PISSN: 08866236     EISSN: None     Source Type: Journal    
DOI: 10.1029/2004GB002256     Document Type: Article

References (43)

1. Akima, H. (1970), A new method of interpolation and smooth curve fitting based on local procedures, J. Assoc. Comput. Mach., 17(4), 589-602.
2. Anderson, L., and J. Sarmiento (1994), Redfield ratios of remineralization determined by nutrient data analysis, Global Biogeochem. Cycles, 8(1), 65-80.
3. Antoine, D., J. M. André, and A. Morel (1996), Oceanic primary production: 2. Estimation at global scale (coastal zone color scanner) chlorophyll, Global Biogeochem. Cycles, 10(1), 57-69.
4. Broecker, W. S. (1974), A conservative water-mass tracer, Earth Planet. Sci. Lett., 23,100-107.
5. Buesseler, K. O., A. F. Michaels, D. A. Siegel, and A. H. Knap (1994), A three-dimensional time-dependent approach to calibrating sediment trap fluxes, Global Biogeochem. Cycles, 8(2), 179-193.
6. Chung, S.-N., K. Lee, R. A. Feely, C. L. Sabine, F. J. Millero, R. Wanninkhof, J. L. Bullister, R. M. Key, and T.-H. Peng (2003), Calcium carbonate budget in the Atlantic Ocean based on water column inorganic carbon chemistry, Global Biogeochem. Cycles, 17(4), 1093, doi:10.1029/ 2002GB002001.
7. Cullen, J. J. (1991), Hypotheses to explain high-nutrient, low chlorophyll conditions in the open sea, Limnol. Oceanogr., 36, 1578-1599.
8. Emery, W. J., and J. Meincke (1986), Global water masses: Summary and review, Oceanol. Acta, 9(4), 383-391.
9. 2 in die Atlantic Ocean, Global Biogeochem. Cycles, 12(1), 165-191.
10. Gruber, N., and J. L. Sarmiento (1997), Global patterns of marine nitrogen fixation and denitrification, Global Biogeochem. Cycles, 11(2), 235-266.
11. Helland-Hansen, B. (1918), Nogen hydrografiske metoder, Forh. Skand. Nat. Møte, 16, 357-359.
12. Hupe, A., and J. Karstensen (2000), Redfield stoichiometry in the Arabian Sea, Global Biogeochem. Cycles, 14(1), 357-372.
13. Intergovernmental Panel on Climate Change (2001), Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change (IPCC), edited by J. T. Houghton et al., Cambridge Univ. Press, New York.
14. Kähler, P., and E. Bauerfeind (2001), Organic particles in a shallow sediment trap: Substantial loss to the dissolved phase, Limnol. Oceanogr., 46, 719-723.
15. Karstensen, J., and D. Quadfasel (2002), Formation of Southern Hemisphere thermocline waters: Water mass conversion and subduction, J. Phys. Oceanogr., 22, 3020-3038.
16. Karstensen, J., and M. Tomczak (1998), Age determination of mixed water masses using CFC and oxygen data, J. Geophys. Res., 103(C9), 18,599-18,610.
17. 2, Limnol. Oceanogr., 46, 964-970.
18. Laws, E. A., P. G. Falkowski, W. O. Smith, and H. Ducklow (2000), Temperature effects on export production in the open ocean, Global Biogeochem. Cycles, 14(4), 1231-1246.
19. Lawson, C. L., and R. J. Hanson (1974), Solving Least Square Problems, Prentice-Hall, Upper Saddle River, N. J.
20. Li, Y.-H., and T.-H. Peng (2002), Latitudinal change of remineralization ratios in the oceans and its implication for nutrient cycles, Global Biogeochem. Cycles, 16(4), 1130, doi:10.1029/2001GB001828.
21. Luyten, J., J. Pedlosky, and H. Stommel (1983), The ventilated thermocline, J. Phys. Oceanogr., 13, 292-309.
22. Marshall, J. C., J. G. Nurser, and R. G. Williams (1993), Inferring the subduction rate and period over the North Atlantic, J. Phys. Oceanogr., 23, 1315-1329.
23. Martin, J. H., G. A. Knauer, D. M. Karl, and W. W. Broenkow (1987), VERTEX: Carbon cycling in the northeast Pacific, Deep Sea Res., 34, 267-286.
24. Minster, J., and M. Boulahdid (1987), Redfield ratios along isopycnal surfaces - A complementary study, Deep Sea Res., 34, 1981-2003.
25. Moran, S. B., M. A. Charette, S. M. Pike, and C. A. Wicklund (1999), Differences in seawater particulate organic carbon concentration in samples collected using small- and large-volume methods: The importance of DOC adsorption to the filter blank, Mar. Chem., 67, 33-42.
26. Noji, T., K. Børsheim, F. Rey, and R. Nortvedt (1999), Dissolved organic carbon associated with sinking particles can be crucial for estimates of vertical carbon flux, Sarsia, 84, 129-135.
27. 2 and its relation to new production, export production, and net community production, Global Biogeochem. Cycles, 18, GB1015, doi:10.1029/2003GB002094.
28. Pearson, K. (1901), On lines and planes of closest fit to systems of points in space, Philos. Mag., 6(2), 559-572.
29. Redfield, A. C., B. C. Ketchum, and F. A. Richards (1963), The influence of organisms on the composition of sea water, in The Sea, vol. 2, edited by N. Hill, pp. 26-77, Wiley-Interscience, Hoboken, N. J.
30. Schlitzer, R. (2000), Applying the adjoint method for global biogeochemical modeling, in Inverse Methods in Biogeochemical Cycles, Geophys. Monogr. Ser., vol. 114, edited by P. Kasibhatla et al., pp. 107-124, AGU, Washington, D. C.
31. Schlitzer, R. (2002), Carbon export fluxes in the Southern Ocean: Results from inverse modeling and comparison with satellite based estimates, Deep Sea Res., Part II, 49, 1623-1644.
32. Schneider, B., R. Schlitzer, G. Fischer, and E.-M. Nöthig (2003), Depth-dependent elemental compositions of particulate organic matter (POM) in the ocean, Global Biogeochem. Cycles, 17(2), 1032, doi:10.1029/ 2002GB001871.
33. 230Th calibration, Deep Sea Res., Part II, 48, 2383-2408.
34. Shaffer, G., J. Bendtsen, and O. Ulloa (1999), Fractionation during remineralization of organic matter in the ocean, Deep Sea Res., Part II, 46, 185-204.
35. Siegenthaler, U., and J. Sarmiento (1993), Atmospheric carbon dioxide and the ocean, Nature, 365, 119-125.
36. Suess, E. (1980), Particulate organic carbon flux in the ocean - Surface productivity and oxygen utilization, Nature, 280, 260-263.
37. Sverdrup, H. U., M. W. Johnson, and R. H. Fleming (1942), The Oceans: Their Physics, Chemistry, and General Biology, Prentice-Hall, Upper Saddle River, N. J.
38. 2 in the Oceans (ISSN 1341-4356), edited by Y. Nojiri, pp. 9-14, Cent. for Global Environ. Res. (NIEST), Tsukuba, Japan.
39. Takahashi, T., W. S. Broecker, and S. Langer (1985), Redfield ratio based on chemical data from isopycnal surfaces, J. Geophys. Res., 90(C4), 6907-6924.
40. Tomczak, M. (1999), Some historical, theoretical and applied aspects of quantitative water mass analysis, J. Mar. Res., 57, 275-303.
41. 2 Survey, in Ocean Circulation and Climate, edited by J. Church, G. Siedler, and J. Gould, pp. 489-521, Elsevier, New York.
42. Weiss, R. F. (1970), On the solubility of nitrogen, oxygen and argon in water and seawater, Deep Sea Res., 17, 721-735.
43. You, Y., and M, Tomczak (1993), Thermocline circulation and ventilation in the Indian Ocean derived from water mass analysis, Deep Sea Res., 40, 13-56.