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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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0343029043
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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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45
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0343900660
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note
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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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