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Ocean Color Chlorophyll Algorithms for SEAWIFS

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TLDR
In this article, a large data set containing coincident in situ chlorophyll and remote sensing reflectance measurements was used to evaluate the accuracy, precision, and suitability of a wide variety of ocean color algorithms for use by SeaWiFS (Sea-viewing Wide Field-of-view Sensor).
Abstract
A large data set containing coincident in situ chlorophyll and remote sensing reflectance measurements was used to evaluate the accuracy, precision, and suitability of a wide variety of ocean color chlorophyll algorithms for use by SeaWiFS (Sea-viewing Wide Field-of-view Sensor). The radiance-chlorophyll data were assembled from various sources during the SeaWiFS Bio-optical Algorithm Mini-Workshop (SeaBAM) and is composed of 919 stations encompassing chlorophyll concentrations between 0.019 and 32.79 μg L−1. Most of the observations are from Case I nonpolar waters, and ∼20 observations are from more turbid coastal waters. A variety of statistical and graphical criteria were used to evaluate the performances of 2 semianalytic and 15 empirical chlorophyll/pigment algorithms subjected to the SeaBAM data. The empirical algorithms generally performed better than the semianalytic. Cubic polynomial formulations were generally superior to other kinds of equations. Empirical algorithms with increasing complexity (number of coefficients and wavebands), were calibrated to the SeaBAM data, and evaluated to illustrate the relative merits of different formulations. The ocean chlorophyll 2 algorithm (OC2), a modified cubic polynomial (MCP) function which uses Rrs490/Rrs555, well simulates the sigmoidal pattern evident between log-transformed radiance ratios and chlorophyll, and has been chosen as the at-launch SeaWiFS operational chlorophyll a algorithm. Improved performance was obtained using the ocean chlorophyll 4 algorithm (OC4), a four-band (443, 490, 510, 555 nm), maximum band ratio formulation. This maximum band ratio (MBR) is a new approach in empirical ocean color algorithms and has the potential advantage of maintaining the highest possible satellite sensor signal: noise ratio over a 3-orders-of-magnitude range in chlorophyll concentration.

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Bridging ocean color observations of the 1980s and 2000s in search of long-term trends

TL;DR: In this article, a comprehensive revision of the Coastal Zone Color Scanner (CZCS) data-processing algorithms has been undertaken to generate a revised level 2 data set from the near-8-year archive (1979-1986) collected during this "proof-of-concept" mission.
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MERIS satellite chlorophyll mapping of oligotrophic and eutrophic waters in the Laurentian Great Lakes

TL;DR: In this paper, a linear relationship was found between Chla concentration and fluorescence line height (FLH) computed with these MERIS bands, and the same relationship held for observations on oligotrophic waters elsewhere, but not for Green Bay, where the FLH diminished to become negative as Chla increased.
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A bio-optical algorithm for the remote estimation of the chlorophyll-a concentration in case 2 waters

TL;DR: In this article, the authors evaluated the performance of a recently developed three-band model and its special case, a twoband model, for the remote estimation of the chlorophyll-a (chl-a) concentration in turbid productive case 2 waters.
Journal ArticleDOI

A Survey on Gaussian Processes for Earth-Observation Data Analysis: A Comprehensive Investigation

TL;DR: In this paper, the main theoretical Gaussian Process (GPs) developments in the field of biogeophysical parameter retrieval are reviewed, considering new algorithms that respect signal and noise characteristics, extract knowledge via automatic relevance kernels, and allow applicability of associated uncertainty intervals to transport GP models in space and time that can be used to uncover causal relations between variables and can encode physically meaningful prior knowledge via radiative transfer model (RTM) emulation.
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Independence and interdependencies among global ocean color properties: Reassessing the bio-optical assumption

TL;DR: In this article, a semi-analytical ocean color algorithm, the Garver-Siegel-Maritorena model (GSM01), was employed to decompose ocean color imagery from the Sea-viewing Wide Field of view Sensor (SeaWiFS) into optically relevant components for phytoplankton absorption (related to the chlorophyll concentration, Chl), colored non-algal absorption and particulate backscatter.
References
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Journal ArticleDOI

Photosynthetic rates derived from satellite‐based chlorophyll concentration

TL;DR: In this paper, a light-dependent, depth-resolved model for carbon fixation (VGPM) was developed to understand the critical variables required for accurate assessment of daily depth-integrated phytoplankton carbon fixation from measurements of sea surface pigment concentrations (Csat)(Csat).
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Fluorometric analysis of chlorophyll a in the presence of chlorophyll b and pheopigments

TL;DR: A fluorometric method is described which provides sensitive measurements of extracted chlorophyll a free from the errors associated with conventional acidification techniques and provides adequate sensitivity for small sample sizes even in the most oligotrophic marine and freshwater environments.
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Analysis of variations in ocean color1

TL;DR: The R(λ) values observed for blue waters are in full agreement with computed values in which new and realistic values of the absorption coefficient for pure water are used and presented.
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