The flow between Hamilton Harbour and Cootes Paradise was monitored from Ap
ril until December 1997 to provide background information for the operation
of a fishway in the connecting channel. The flow was highly variable, and
changed direction several times each day. Comparison with local meteorologi
cal and water level data revealed several interesting features. Outflow eve
nts of 4 hours or greater in duration were typically preceded by winds from
the east usually lasting at least 6 hours. Similarly inflow events longer
than 4 hours were typically preceded by westerly winds for at least 6 hours
. There was evidence of diurnal and semi-diurnal flow reversals and of free
surface oscillations of Lake Ontario, but not of Helmholtz resonance betwe
en Hamilton Harbour and the lake nor of exchange flow resonance between the
harbor and Cootes Paradise.