A two-layer, coupled physical-biological model was used to investigate
phytoplankton dynamics in the north-western Irish Sea. The model was
parameterized with values obtained from the published literature, and
predicted the concentration of chlorophyll and dissolved inorganic nit
rogen in an upper and lower layer. Simulations were driven with measur
ed hourly values of meteorological data. The timings of the spring blo
om predicted by the model at a summer thermally stratified site and a
vertically mixed site were compared with observations made during 1992
. At the mixed site, good agreement was found between the model and ob
servations. At the stratified site, the results are less satisfactory
and show that the model predicted a spring bloom 13 days later than ob
served. The difference was probably due to overestimation of the surfa
ce mixed-layer depth leading to underestimation of upper-layer irradia
nce. A simple numerical experiment demonstrated that the timing of the
spring bloom was best simulated using the maximum theoretically justi
fiable value for photosynthetic efficiency.