Using the location, data, and water levels from flood events along the
Canadian shore of Great Lakes, flood damage thresholds were determine
d to identify and compare water levels at which static and storm-induc
ed high water impact shoreline interests on several shore reaches of L
ake Erie, Huron, Ontario, and St. Clair. Spatial differences identifie
d may be related to several factors, including: 1) nearshore bathymetr
ies; 2) extent of residential development along low-lying shorelines;
3) degree of riparian adjustment to flooding; and 4) location relative
to dominant wind or storm directions. Correlation analyses found that
flood damage levels are more closely correlated to fluctuations in st
atic levels on Lakes Ontario, Huron, and St. Clair, while flood damage
levels are more closely correlated to maximum instantaneous water lev
els on Lake Erie. Correlation analyses of individual gauge data identi
fied locations possibly more susceptible to storm surges. A conservati
ve approach to determining flood damage thresholds is suggested, being
based on a standard deviation below the mean of maximum instantaneous
flood levels for a given gauge. The standard deviation threshold, whi
le lower than current ''critical levels'' used in management, is more
representative of the majority of flood damage levels than thresholds
based on lowest maximum instantaneous lake levels. However, caution is
urged in applying any critical level solely based on water level gaug
e information as Great Lakes flooding is a highly site-specific phenom
enon influenced by meteorologic factors.