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David Antoine

Researcher at Curtin University

Publications -  135
Citations -  9241

David Antoine is an academic researcher from Curtin University. The author has contributed to research in topics: Ocean color & SeaWiFS. The author has an hindex of 43, co-authored 122 publications receiving 8146 citations. Previous affiliations of David Antoine include University of Paris & Centre national de la recherche scientifique.

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Oceanic primary production: 2. Estimation at global scale from satellite (Coastal Zone Color Scanner) chlorophyll

TL;DR: In this article, a fast method has been proposed to compute the oceanic primary production from the upper ocean chlorophyll-like pigment concentration, as it can be routinely detected by a spaceborne ocean color sensor.
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A comparison of global estimates of marine primary production from ocean color

TL;DR: The third primary production algorithm round robin (PPARR3) as discussed by the authors compares output from 24 models that estimate depth-integrated primary production from satellite measurements of ocean color, as well as seven general circulation models (GCMs) coupled with ecosystem or biogeochemical models.
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Seasonal and interannual variability in algal biomass and primary production in the Mediterranean Sea, as derived from 4 years of SeaWiFS observations

TL;DR: In this paper, the seasonal cycles of algal biomass generally reveal a maximum in winter or spring, and a minimum in summer, and the seasonal evolution of primary production is predominantly influenced by that of alga biomass in the Western Basin with, in particular, a spring maximum.
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Bidirectional reflectance of oceanic waters: accounting for Raman emission and varying particle scattering phase function

TL;DR: The bidirectionality of the upward radiance field in oceanic case 1 waters has been reinvestigated by incorporation of revised parameterizations of inherent optical properties as a function of the chlorophyll concentration, considering Raman scattering and making the particle phase function shape continuously varying along with the Chl.