Storm Surge Hazard in Canada

Storm surges occur frequently in Canada mainlydue to extra-tropical cyclones (ETC'S) also referred to as winter storms. The hurricanes from the Gulf of Mexico can affect eastern Canada including Lakes Ontario and Erie regions, after they get modified and acquire some extra-tropical characteristics. Storm surges have occurred both on the Atlantic and Pacific coasts, in the Gulf of St.Lawrence, St.Lawrence Estuary, Bay of Fundy, Hudson Bay, James Bay, Northwest Passage, Beaufort Sea, the Great Lakes and other large lakes such as Lake Winnipeg.Squall lines which are embedded in the largerscale synoptic systems like the ETC'S could also generate storm surges (referred to as edge waves) in Lakes Huron, Erie and Ontario (edge waves are most prominent in Lake Michigan, but Canada has no territory touching this lake). The effect of climate change on storm surges in the Canadian water bodies could be two-fold. First, there may be some possible intensification of the weather systems and the associated wind fields resulting in bigger surges. Second, and probably even more relevant, is an east-west and north-south shift in the tracks of the weather systems, which could expose certain new areas to storm surge activity.A high priority for proper assessment of storm surge hazard is the production of maps showing inundation zones for storm surges that might occur in populated coastal areas. Such maps can be used to improve public awareness of tsunamis and for planning purposes (i.e., to reduce or avoid the risk).

[1]  J. F. Keers.  An empirical investigation of interaction between storm surge and astronomical tide on the east coast of Great Britain , 1968 .

[2]  P. Hamblin.  Seiches, Circulation, and Storm Surges of an Ice-Free Lake Winnipeg , 1976 .

[3]  Maurice Danard,et al.  Inclusion of ice cover in a storm surge model for the Beaufort Sea , 1989 .

[4]  David A. Greenberg,et al.  Numerical simulation of the storm surge of January 1982 on the south coast of Newfoundland , 1987 .

[5]  J. Rossiter.  Interaction Between Tide and Surge in the Thames , 1961 .

[6]  G. McBean,et al.  Explosive Cyclogenesis over the Northeast Pacific Ocean , 1983 .

[7]  T. Healy,et al.  New Zealand tsunamis 1840–1982 , 1986 .

[8]  M. Danard,et al.  Storm surge mitigation through vegetation canopies , 1994 .

[9]  Douglas K. Maurer,et al.  Effects of Storm Surges on the Beaufort Sea Coast, Northern Alaska , 1979 .

[10]  O. Cramer,et al.  The Columbus Day “Big Blow” in Oregon , 1962 .

[11]  J. Wolf,et al.  The interaction of surge and tide in the North Sea and River Thames , 1978 .

[12]  J. Proudman.  The effect of friction on a progressive wave of tide and surge in an estuary , 1955, Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences.

[13]  G. Platzman,et al.  AN INVESTIGATION OF THE METEOROLOGICAL CONDITIONS ASSOCIATED WITH EXTREME WIND TIDES ON LAKE ERIE , 1962 .

[14]  T. Murty,et al.  Influence of an ice layer on the propagation of long waves , 1979 .

[15]  R. Lawford,et al.  The Southern Ontario Blizzard of January 26 and 27, 1978 , 1979 .

[16]  M. Danard,et al.  Storm surges in Canadian waters , 1995 .

[17]  Robert L. Jones,et al.  Canadian disasters: An historical survey , 1992 .

[18]  H. Lamb.  Climate: present, past and future , 1977 .

[19]  M. I. El-Sabh,et al.  Statistics of Extreme Storm Surges in Eastern Canadian Waterbodies , 1981 .

[20]  Tad Murty,et al.  Storm surges : meteorological ocean tides , 1984 .