We formulate a strategic simulation model of a fjordic ecosystem, payi
ng careful attention to consistency of spatial and temporal scales. Ou
r model incorporates all the major physical and biological elements of
the system but is simple enough to allow unambiguous identification o
f the mechanisms underlying its behavior. Despite this simplicity the
model is capable of semiquantitative agreement with the observed behav
ior of the Killary Harbor ecosystem over the 1981 season. The key conc
lusion from our analysis of the model is that because of the very high
rates of tidal and freshwater flushing in Scottish sea-lochs, the per
sistence of such systems is ultimately determined by the balance of nu
trient import and export in a manner analogous to a laboratory chemost
at. Except at the peak of the spring bloom, inorganic nitrogen supply
exceeds biological demand, so that primary production is controlled by
physical factors (temperature and irradiance) and the activities of h
igher trophic levels. The size of the spring phytoplankton bloom is ma
inly determined by the dynamics of the following zooplankton bloom and
is thus strongly influenced by the over-wintering success of zooplank
ton inside the system as well as zooplankton immigration from the sea.