| Literature DB >> 20720921 |
Toby K Westberry1, Giorgio Dall'Olmo, Emmanuel Boss, Michael J Behrenfeld, Thierry Moutin.
Abstract
We present an extensive data set of particle attenuation (c(p)), backscattering (b(bp)), and chlorophyll concentration (Chl) from a diverse set of open ocean environments. A consistent observation in the data set is the strong coherence between c(p) and b(bp) and the resulting constancy of the backscattering ratio (0.010 +/- 0.002). The strong covariability between c(p) and b(bp) must be rooted in one or both of two explanations, 1) the size distribution of particles in the ocean is remarkably conserved and particle types responsible for c(p) and b(bp) covary, 2) the same particle types exert influence on both quantities. Therefore, existing relationships between c(p) or Chl:c(p) and phytoplankton biomass and physiological indices can be conceptually extended to the use of b(bp). This finding lends support to use of satellite-derived Chl and b(bp) for investigation of phytoplankton biomass and physiology and broadens the applications of existing ocean color retrievals.Entities:
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Year: 2010 PMID: 20720921 DOI: 10.1364/OE.18.015419
Source DB: PubMed Journal: Opt Express ISSN: 1094-4087 Impact factor: 3.894