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The Martin curve is a power law used by oceanographers to describe the export to the ocean floor of particulate organic carbon (POC). The curve is controlled with two parameters: the reference depth in the water column, and a remineralisation parameter which is a measure of the rate at which the vertical flux of POC attenuates. It is named after the American oceanographer John Martin.

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  • Martin curve (en)
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  • The Martin curve is a power law used by oceanographers to describe the export to the ocean floor of particulate organic carbon (POC). The curve is controlled with two parameters: the reference depth in the water column, and a remineralisation parameter which is a measure of the rate at which the vertical flux of POC attenuates. It is named after the American oceanographer John Martin. (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/POC.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Pelagiczone.svg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Effective_Martin_curve_slope_for_POC.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Flux_of_POC_with_depth.png
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  • The Martin curve is a power law used by oceanographers to describe the export to the ocean floor of particulate organic carbon (POC). The curve is controlled with two parameters: the reference depth in the water column, and a remineralisation parameter which is a measure of the rate at which the vertical flux of POC attenuates. It is named after the American oceanographer John Martin. (en)
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