We examined blooms of the coccolithophorid E. huxleyi, observed in SeaWiFS
imagery, with a new algorithm for the retrieval of detached coccolith conce
ntration. The algorithm uses only SeaWiFS bands in the red and near infrare
d (NIR) to minimize the influence of the absorption by chlorophyll and diss
olved organic material. We used published experimental determinations of th
e calcite specific backscattering and its spectral dependence, and assumed
that the absorption coefficient of the medium was that of pure water, to es
timate the marine contribution to the SeaWiFS radiance. The aerosol land Ra
yleigh-aerosol interaction) contribution to the radiance was modeled as an
exponential function of wavelength. These allow derivation of the coccolith
concentration on a pixel-by-pixel basis from SeaWiFS imagery. Application
to a July 30, 1999 SeaWIFS image of a bloom south of Plymouth, UK indicates
that the SeaWiFS estimates are in good agreement with surface measurements
of coccolith concentration.