INTERANNUAL VARIABILITY OF THE EARLY-LIFE HISTORY OF WALLEYE POLLOCK NEAR SHELIKOF-STRAIT AS INFERRED FROM A SPATIALLY EXPLICIT, INDIVIDUAL-BASED MODEL
Aj. Hermann et al., INTERANNUAL VARIABILITY OF THE EARLY-LIFE HISTORY OF WALLEYE POLLOCK NEAR SHELIKOF-STRAIT AS INFERRED FROM A SPATIALLY EXPLICIT, INDIVIDUAL-BASED MODEL, Fisheries oceanography, 5, 1996, pp. 39-57
A coupled biophysical model is used to hindcast the early life history
of a population of walleye pollock (Theragra chalcogramma), to assess
possible physical causes of interannual Variability in recruitment. T
he modelling approach combines a primitive equation, rigid-lid hydrody
namic model with a probabilistic, individual-based biological model of
growth, development, and mortality. Individuals are tracked through s
pace using daily velocity fields generated from the hydrodynamic model
, along with self-directed vertical migrations appropriate to each lif
e stage in the biological model. The hydrodynamic model is driven with
wind and runoff time series appropriate to each year. Biological mode
l output compares favourably with observed spatial distributions for s
pecific years. Lloyd's index of patchiness, calculated from model outp
ut, was similar to values calculated from field data. Five noncontiguo
us years were chosen for hindcasts to span a wide range of meteorologi
cal conditions (winds, runoff) and recruitment success. Interannual co
mparisons suggest that two years of above average recruitment (1978 an
d 1988), and one year of below average recruitment (1991), experienced
flow fields which carried many individuals into the Alaskan Stream. A
t the same time, the vigorous flow fields generated in each of these y
ears carried some individuals onto the shelf area to the south-west of
the spawning site. A year with low runoff and weak winds (1989) exhib
ited weak circulation, with extended retention of larvae near the spaw
ning site. A year with high runoff (1987) was notable for the strength
and frequency of mesoscale eddy activity. Eddies appear capable of bo
th enhancing patchiness of early larvae (through retention) and dissip
ating patchiness of juveniles (through mesoscale mixing), Larvae retai
ned in an eddy feature exhibit a narrower range of sizes than the popu
lation outside that feature.