Abstract
Negative storm surges in eastern Canadian water bodies are studied. These water bodies include the Atlantic Coast of Canada, the Labrador Sea Coast, Bay of Fundy, Gulf of St. Lawrence and St. Lawrence estuary. Using hourly observed and predicted sea level variations for a period of eleven years (1956—1975), statistical analyses were made to examine the extreme values, the return periods for negative surges of various amplitudes, the influence of an ice layer and the interaction between tides and surges. The analysis for the Labrador coast, Bay of Fundy and Gulf of St. Lawrence shows that negative surges with amplitudes up to 1.7 m have occurred during the 11-yr period of study at Pointe-du-Chêne. The negative surges generally are greater where strong and abrupt water depth changes occur. Largest negative surges occurred in winter, and smallest negative surges occurred in summer. This is due in part, to the presence of ice cover and, in part, to the fact that the weather systems that generate these surges are much stronger in winter than in summer. In these regions, the return periods of the extreme surges vary between 1 and 11 yr, but usually are less than 5 yr for most of the stations. Extreme values for negative surges in the St. Lawrence estuary are, in general, greater than for the other regions considered, with maximum value of 2.2 m observed at Québec. All other locations in the upper estuary have amplitudes with value of 1.4 m between 1.8 and 1.9 m. The smallest amplitude negative surges occurred at Pointe-au-Père and Baie- Comeau. In terms of frequency, the negative surges are most prominent at St-FranÇois and least prominent at Ste-Anne-des-Monts. Based on the amplitudes and frequencies for both positive and negative surges, we conclude that stations located at the lower part of the estuary (Pointe-au-Père, Baie-Comeau, Rivière-du- Loup) are reasonably safe from storm surges, while Québec City and St-FranÇois are extremely prone to storm surges. However, one reassuring feature at Québec City and St-FranÇois is that positive surges occur mostly at the time of low tide while negative surges occur at the time of high tide. On the other hand, at St- Jean-Port-Joli and St-Joseph-de-la-Rive positive surges occur at the time of high tide, which is a factor that makes the overall water level variations at these locations quite significant. Similar behaviour of the tidal wave propagation in the estuary and that of storm surge amplitudes is demonstrated.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
El-Sabh, M. I., Murty, T. S., and Briand, J.-M.: 1984, ‘Les Ondes de TempÄte dans l’Estuaire du Saint- Laurent’, Sci. Tech, de l’Eau 17, 15–22.
Geelhoed, P. T.: 1973, ‘Negative Surges in the Southern North Sea’, Int. Hydrogr. Rev. 50, 61–73.
Henry, R. F.: 1975, ‘Storm Surges’, Dept of Environment, Victoria, B.C., Canada. Tech. Rep. no. 19, Beaufort Sea Project, 41 p.
Keers, J. F.: 1968, ‘An Empirical Investigation of Interaction between Storm Surges and Astronomical Tide on the East Coast of Great Britain’, Deutsche Hydrogr. Zeits 21,118–128.
Lisitzin, E.: 1974, Sea Level Changes. Elsevier Oceanogr. Series No. 8, New York, N.Y., 273 p.
Murty, T. S.: 1984, ‘Storm Surges Meteorological Ocean Tides’, Can., Bull. Fish. Aquat. Sci. 212, 897 p.
Murty, T. S. and El-Sabh, M. I.: 1981, ‘Interaction between Storm Surges and Tides in Shallow Waters’, Mar. Geodesy 5,19–33.
Murty, T. S. and Holloway, G.: 1985, ‘Influence of Marginal Ice Cover on Storm Surges’, J. Waterway Port Coastal Ocean Eng., American Soc. Civil Engineers, N.Y., Vol. 11(2), 329–336.
Murty, T. S. and Polavarapu, R. J.: 1979, ‘Influence of an Ice Layer on the Propagation of Long Waves’, Mar. Geodesy 2, 99–125.
Murty, T. S., El-Sabh, M. I., and Briand, J.-M.: 1979, ‘Storm Surge Amplitudes in the St. Lawrence Estuary’, J. Can. Hydrogr. Assoc. 20, 8–10.
Murty, T. S., El-Sabh, M. I., and Briand, J.-M.: 1981a, ’Statistics of Extreme Storm Surges in Eastern Canadian Water Bodies’, pp. 1184–1188. Proc. Oceans-81 Conf, Sept. 16–18, 1981, Boston, MA. Inst. Electrical and Electronics Engineers, New York, N.Y., 1222 p.
Murty, T. S., El-Sabh, M. I., and Briand, J.-M.: 1981b, ’Influence of an Ice Layer on Storm Surge Amplitudes’, Proc. Int. Conf Maritime Engineerings in the Arctic Ocean, Quebec, Que. Laval University, Vol. 1,415–421.
Prandle, D. and Wolf, J.: 1978, ‘Surge-tide Interaction in the Southern North Sea’, Hydrodynamics of Estuaries and Fjords, Elsevier Oceanogr. Series no. 23,161–185.
Proudman, J.: 1955, ‘The Propagation of Tide and Surge in an Estuary’, Proc. Royal Soc. London, Ser. A 231,8–24.
Rossiter, J. R.: 1961, ’Interaction between Tide and Surge in the Thames’, Geophys. J. Royal Astronomical Soc. 6, 29–53.
Rossiter, J. R.: 1971, ’Long-period Waves: Seiches, Surges and Tides in Coastal Waters, pp. 155–168. In: D. A. Howells, I. P. Haigh and C. Tayler (eds.), Dynamics of Waves in Civil Engineering, Wiley Inter- science, New York, N.Y., 575 p.
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1988 D. Reidel Publishing Company
About this paper
Cite this paper
El-Sabh, M.I., Murty, T.S., Briand, JM. (1988). Negative Storm Surges on Canada’s East Coast. In: El-Sabh, M.I., Murty, T.S. (eds) Natural and Man-Made Hazards. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-1433-9_22
Download citation
DOI: https://doi.org/10.1007/978-94-009-1433-9_22
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-7142-0
Online ISBN: 978-94-009-1433-9
eBook Packages: Springer Book Archive