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Volumn 287, Issue 5454, 2000, Pages 831-833

Temporal trends in deep ocean Redfield ratios

Author keywords

[No Author keywords available]

Indexed keywords

CARBON; NITROGEN; PHOSPHORUS;

EID: 0034603088     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.287.5454.831     Document Type: Article
Times cited : (99)

References (45)
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    • note
    • 2) by 1.2 and 2 mol for each mole of increase in C and N, respectively (33, 34): (AOU:P) δ(AOU:P) = 1.2(C:P) δ(C:P) + 2(N:P) δ(N:P) ⇔ δ(C:P) = [(AOU:P) δ(AOU:P) -2(N:P) δ(N:P)]/[1.2(C:P)] and δ(C:N) = δ(C:P) - δ(N:P) where δ(N:P) = {[1 + δ(AOU:P)]/[1 + δ(AOU:N)]} - 1.
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    • 1 is the precision of a single measurement.
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    • For each comparison, we collected AOU, S, and T data on the same density surface, within up to 5° latitude and longitude of the location, and calculated the regression of AOU versus S and AOU versus T. We then used these regressions to estimate the possible change in AOU due to the variations in S and T.
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    • Adjusting the results for this potential change would increase the observed trends. Therefore, to ensure that the results remain conservative, we did not apply this adjustment.
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    • t1 from 8 to 14 resulted in differences of <0.13 per mil per year in the reported trends.
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    • note
    • Supported in part by the project Marine Ecosystems Regulation: Trace Metal and Carbon Dioxide Limitations (MERLIM) of the European Union within the Marine Science and Technology Programme under Contract MAS3-CT95-0005. We thank D. A. Wolf-Gladrow, A. Wischmeysr, R. Schlitzer, R. Gerdes, P. Falkowski, and T. Tyrrell for stimulating discussions on the topic and S. Burkhardt for helpful comments on an earlier version of this manuscript This study would not have been possible without the work of all people aboard the research vessels who collected the nutrient data and made them accessible. This is publication 1736 of the Alfred Wegener Institute for Polar and Marine Research.


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