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  • Articles  (2)
  • Wiley  (2)
  • Kiel: Kiel Institute for the World Economy (IfW)
  • Geophysical Research Letters  (2)
  • 4905
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  • Articles  (2)
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  • 1
    Publication Date: 2013-02-16
    Description: [1]  Phytoplankton are an important component of the oceanic carbon cycle. Yet, due to methodological constraints, the carbon biomass of phytoplankton is poorly characterised. To address this limitation, we have explored the bio-optical relationship between in-situ measurements of the particle backscattering coefficient at 470 nm, b bp (470), and the phytoplankton carbon concentration for cells with diameter less than 20  μ m (C f ). We found a significant relationship between b bp (470) and C f for Atlantic oceanic waters with chlorophyll-a concentrations less than 0.4 mg m -3 (or b bp (470) 〈 0.003 m -1 ). This relationship could be used to estimate C f from data collected by in-situ autonomous platforms and from remote sensing of ocean colour.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 2
    Publication Date: 2017-06-28
    Description: We explore a novel and spatially extensive dataset obtained from Biogeochemical-Argo (or BGC-Argo) floats, containing 16,796 profiles of the particulate backscattering coefficient at 700nm ( b b p (700)) measured with three different sensors. We focus at the 900-950m depth interval (within the mesopelagic), where we blackfound values to be relatively constant. While we find significant differences between estimates of b b p (700) obtained with different sensors (≈30 % disagreement), the median values in most oceanic regions obtained with blacka single type of sensor are within 50 % of each other and are consistent with measurements of suspended mass conducted in the early 1970's. Deviations from the quasi-constant background value likely indicate times and locations associated with higher particulate export to depth. Indeed, we observe that in productive high latitude regions, a deep seasonal signal is observed, with enhanced values recorded blacka few months after surface spring/summer maximal concentrations. In addition, the deep b b p (700) is highest in regions exhibiting suboxic-anoxic conditions (e.g. Northern Indian Ocean), which have been associated with local particulate production as well as reduced particle flux attenuation.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
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