We use autonomous nitrate (NO3−), oxygen (O2), and dissolved inorganic carbon (DIC) observations to examine the relationship between ratios of C:N:O at an upwelling site in the Southern California Current System. Mean ratios and 95% confidence intervals observed by sensors over 8 months were NO3−:O2 = −0.11 ± 0.002, NO3−:DIC = 0.14 ± 0.001, and DIC:O2 = −0.83 ± 0.01, in good agreement with Redfield ratios. Variability in the ratios on the weekly time scale is attributable to shifts in biological demand and nutrient availability and shown to exhibit a spectrum of values ranging from near 100% New Production to 100% Regenerated Production.
Dynamic variability of biogeochemical ratios in the Southern California Current System
- Author(s): Todd Martz, Uwe Send, Mark D. Ohman, Yuichiro Takeshita, Philip Bresnahan, Hey-Jin Kim, SungHyun Nam
- Geophysical Research Letters
- March 22, 2014
Citation: Martz, T., U. Send, M. D. Ohman, Y. Takeshita, P. Bresnahan, H.-J. Kim, and S. H. Nam (2014), Dynamic variability of biogeochemical ratios in the Southern California Current System, Geophys. Res. Lett., 41, 2496–2501, doi:10.1002/2014GL059332.