Carbon to chlorophyll-a ratio (CCHL) is formulated based on the assumption
that adaptive changes in carbon to chlorophyll occur so as to maximize the
specific growth rate for ambient conditions, including solar radiation and
water temperature. With the dynamic CCHL, an unsteady two-layered, two-dime
nsional eutrophication numerical model for density stratified coastal water
s has been developed. Saturated light intensity (Is) is determined as weigh
ted average of the light intensity for previous three days to incorporate l
ight acclimation by phytoplankton. The bottom water anoxic condition during
summer in Tolo Harbour, Hong Kong is successfully reproduced by the presen
t method. Otherwise, the simulation with a constant CCHL gave a wrong resul
t. (C) 1998 IAWQ Published by Elsevier Science Ltd. All rights reserved.