Physics – Optics
Scientific paper
Mar 2004
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004georl..3106305m&link_type=abstract
Geophysical Research Letters, Volume 31, Issue 6, CiteID L06305
Physics
Optics
6
Oceanography: Biological And Chemical: Plankton, Oceanography: Biological And Chemical: Photochemistry, Oceanography: Biological And Chemical: Optics
Scientific paper
The compensation irradiance for phytoplankton is calculated from the time course of fluorescence-derived chlorophyll-a measured on moored sensors in the North Atlantic in spring. Following the initiation of the spring bloom, the time at which chlorophyll-a begins to decrease at a particular depth in a stratified water column is used to compute the compensation irradiance from the critical depth criterion. Over the depth range of 50-110 m, the compensation irradiance is estimated to be in the range from 0.1-0.3 mol photons m-2 d-1.
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