Wp. Bissett et al., THE EFFECTS OF TEMPORAL VARIABILITY OF MIXED-LAYER DEPTH ON PRIMARY PRODUCTIVITY AROUND BERMUDA, J GEO RES-O, 99(C4), 1994, pp. 7539-7553
Temporal variations in primary production and surface chlorophyll conc
entrations, as measured by ship and satellite around Bermuda, were sim
ulated with a numerical model. In the upper 450 m of the water column,
population dynamics of a size-fractionated phytoplankton community we
re forced by daily changes of wind, light, grazing stress, and nutrien
t availability. The temporal variations of production and chlorophyll
were driven by changes in nutrient introduction to the euphotic zone d
ue to both high- and low-frequency changes of the mixed layer depth wi
thin 32-degrees-34-degrees-N, 62-degrees-64-degrees-W between 1979 and
1984. Results from the model derived from high-frequency (case 1) cha
nges in the mixed layer depth showed variations in primary production
and peak chlorophyll concentrations when compared with results from th
e model derived from low-frequency (case 2) mixed layer depth changes.
Incorporation of size-fractionated plankton state variables in the mo
del led to greater seasonal resolution of measured primary production
and vertical chlorophyll profiles. The findings of this study highligh
t the possible inadequacy of estimating primary production in the sea
from data of low-frequency temporal resolution and oversimplified biol
ogical simulations.