S. Sagan et al., THE RELATIONSHIP BETWEEN BEAM ATTENUATION AND CHLOROPHYLL CONCENTRATION AND REFLECTANCE IN ANTARCTIC WATERS, Deep-sea research. Part 2. Topical studies in oceanography, 42(4-5), 1995, pp. 983-996
Optical and biological data collected during the two-month R.R.S Disco
very expedition in Antarctic waters in the Austral spring were used to
examine the relationships between c(660 nm), chlorophyll a and the re
flectance ratios R(443)/R(550), R(490)/R(550) and R(443 nm). Values of
(c-c(w))(660 nm) varied from 0.20 to 1.2 m(-1), being generally posit
ively correlated with the chlorophyll concentration. The computed valu
es of the pigment specific beam attenuation coefficient c were greate
r than those typical in Case I waters, exceeding 0.9 m(2) mg(-)1, redu
cing the accuracy of the chlorophyll remote sensing algorithms designe
d for Case I waters. The covariance of phytoplankton and related pigme
nts with beam attenuation was examined by the regression equation c-c(
w)= A + B(Chl a + phaeo), and the residuals were used to identify the
non-chlorophyll dependent data in the region. When the non-chlorophyll
dependent data were removed, the accuracy of the chlorophyll remote s
ensing model was significantly improved.