Optical backscattering is correlated with phytoplankton carbon across the Atlantic Ocean
Version of Record online: 21 MAR 2013
©2013. American Geophysical Union. All Rights Reserved.
Geophysical Research Letters
Volume 40, Issue 6, pages 1154–1158, 28 March 2013
How to Cite
2013), Optical backscattering is correlated with phytoplankton carbon across the Atlantic Ocean, Geophys. Res. Lett., 40, 1154–1158, doi:10.1002/grl.50252., , , , and (
- Issue online: 27 APR 2013
- Version of Record online: 21 MAR 2013
- Accepted manuscript online: 15 FEB 2013 01:32PM EST
- Manuscript Accepted: 11 FEB 2013
- Manuscript Revised: 7 FEB 2013
- Manuscript Received: 27 NOV 2012
All Supporting Information may be found in the online version of this article.
|grl50252-sup-0001-README.txt||plain text document||1K||grl50252-sup-0001-README.txt|
|grl50252-sup-0002-Supplementary_Methods.pdf||PDF document||249K||Supporting Information|
|grl50252-sup-0003-Supplementary_Fig1.PDF||PDF document||235K||Fractional contribution of each phytoplankton type to Cf. N is the number of samples used to calculate the median and the standard deviation of the mean for each type of phytoplankton for three bbp(470) categories.|
|grl50252-sup-0004-Supplementary_Table1.pdf||PDF document||88K||Median relative contributions (%) to Cf by phytoplankton group (i). The data used to construct these tables are from samples with bbp(470) < 0.003 m−1 and within 1.5Zeu. Results shown are divided in four groups: all the dataset, temperate, oligotrophic, and equatorial regions, according to Tarran et al. .|
|grl50252-sup-0005-Supplementary_Table2.pdf||PDF document||83K||Median relative contributions (%) to the total uncertainty (σ2(Cf)) due to the uncertainty (σ2(Cf,x)) in each input parameter (i.e., x = N(i,j), ε(i) or D(i)). The uncertainty in Cf,x presented by phytoplankton group (i), for phytoplankton groups that contribute to 5% or more of Cf (Supplementary Table Error! Reference source not found.). The corresponding spaces have been left blank to facilitate readability. The data used to construct these tables are from samples with bbp(470) < 0.003 m−1 and within 1.5Zeu. Results are shown are divided in four groups: all the dataset, temperate, oligotrophic, and equatorial regions, according to Tarran et al. .|
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