Changes in spectral irrad~ance beneath annual sea ice were measured during the development of sea ice microalgal communities in McMurdo Sound, Antarctica. Five different light regimes were initially estabhshed by varying surface snow cover on 10 m X 10 m sea ice quadrats. The presence of ice algae in quadrats w t h 6 5 cm snow cover was indicated by a spectral shift with increased attenuation between 400 and 550 nm and at 671 nm, wavelengths absorbed by diatom pigments. Snow cover had a profound effect on both the rate of community development and community loss by ice ablation. A simple model of factors determining changes in ice algal biomass is described.
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Palmisano et al. (1987) studied this question.