In April 1998 a research cruise was carried out in the Mozambique Channel t
aking detailed optical, water quality and salinity measurements; the Zambez
i plume waters were apparent through strong colour fronts with green waters
in the plume and clear blue waters offshore. A good (r(2) = 0.76) negative
empirical relationship was found between the salinity (S) and yellow subst
ance, represented by the absorption of filtered samples at 440 nm (g440). A
n empirical relationship was found between the salinity and a reflectance r
atio:
S(1/2Z(sd)) = 37.45-7.07 (R555/R490)
An optical model in which light absorption is dominated by yellow substance
and light scattering by inorganic particles confirms this empirical relati
onship. This has been applied to a SeaWIFS image to map salinity on the Sof
ala Bank, demonstrating the potential to remotely determine the distributio
n of the Zambezi River plume. It is thought that any significant level of c
hlorophyll would reduce the effectiveness of the above algorithm. (C) 2001
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