POTENTIAL IMPACTS OF GLOBAL SEA‐LEVEL RISE ON CANADIAN COASTS

The sea-level rise that may result from global climate change is placed within the context of past and present sea-level changes on Canadian coasts. To assess future impact, a dimensionless index of sensitivity is determined. Coasts with low, moderate, and high sensitivity constitute 67%, 30%, and 3% of the total coastline, respectively. The most sensitive regions are: (1) several parts of the Maritime Provinces; (2) two areas of the British Columbia coast; and (3) a large part of the Beaufort Sea coast. Impacts in four regions - Bay of Fundy, Beaufort Sea, Fraser Delta, and Eastern Shore of Nova Scotia - are discussed in detail. It is argued that the societal response to changes in sea level should favour retreat and accommodation strategies. Il est possible que les changements climatiques globaux provoqueront une elevation du niveau de la mer. Nous examinons ce scenario dans le contexte des changements passes et presents du niveau de la mer sur les cotes canadiennes. Pour evaluer l'impact de l'elevation prevue un indice non dimensionnel de vulnerabilite est determine. Les cotes a la vulnerabilite basse, moderee et elevee constituent, respectivement, 67%, 30%, et 3% de tout le littoral. Les regions les plus vulnerables sont: (1) plusieurs regions dans les provinces maritimes; (2) deux zones sur la cote de la Colombie britannique; et (3) la plupart de la cote de la mer de Beaufort. Nous discutons en detail les impacts dans quatre regions, soit la baie Fundy, la mer Beaufort, la delta du Fraser et la rivage dit ‘Eastern Shore’ de la Nouvelle-Ecosse. Nous estimons que la reponse sociale aux changements du niveau de la mer devrait favoriser des strategies de retraite et d'accommodement.

[1]  Philip R. Hill,et al.  A sea-level curve for the Canadian Beaufort Shelf , 1985 .

[2]  J. Shaw,et al.  Hurricane Hortense strikes Atlantic Nova Scotia: an examination of beach response and recovery , 1997 .

[3]  J. Shaw,et al.  Late Quaternary sedimentation and the postglacial sea-level minimum in Port au Port Bay and vicinity, west Newfoundland , 1993 .

[4]  Julian D. Orford,et al.  Coarse clastic barrier environments: Evolution and implications for quaternary sea level interpretation , 1991 .

[5]  S. Jennings,et al.  Morphodynamic evolution, self-organisation, and instability of coarse-clastic barriers on paraglacial coasts , 1995 .

[6]  P. Vaníček,et al.  A comparison of present sea level linear trends from tide gauge data and radiocarbon curves in Eastern Canada , 1988 .

[7]  Herb Dragert,et al.  Continuous GPS monitoring of elastic strain in the Northern Cascadia Subduction Zone , 1995 .

[8]  John Shaw,et al.  Sensitivity of the Canadian coast to sea-level rise , 1994 .

[9]  S. Solomon,et al.  Influence of ground ice and permafrost on coastal evolution, Richards Island, Beaufort Sea coast, N.W.T. , 1996 .

[10]  John J. Clague,et al.  Postglacial deltaic sediments, southern Fraser River delta, British Columbia , 1991 .

[11]  Philip R. Hill,et al.  Geomorphologic and sedimentary evolution of a transgressive thermokarst coast, Mackenzie delta region, Canadian Beaufort Sea , 1999 .

[12]  M. C. Roberts,et al.  Holocene sea-level change and delta growth: Fraser River delta, British Columbia , 1989 .

[13]  J. Shaw,et al.  Sensitivity of the coasts of Canada to sea-level rise , 1998 .

[14]  J. Allen Salt-marsh growth and fluctuating sea level: implications of a simulation model for Flandrian coastal stratigraphy and peat-based sea-level curves , 1995 .

[15]  J. Shaw,et al.  Shorelines and Rising Sea Levels in Eastern Canada , 1989 .

[16]  Philip R. Hill,et al.  Holocene sea-level history of the Canadian Beaufort shelf , 1993 .

[17]  W. Pilkey,et al.  The concept of shoreface profile of equilibrium: a critical review , 1993 .

[18]  V. Gornitz Global coastal hazards from future sea level rise , 1991 .

[19]  M. Ruz,et al.  A model of coastal evolution in a transgressed thermokarst topography, Canadian Beaufort Sea , 1992 .

[20]  R. Boyd,et al.  CHAPTER 4 – An Evolutionary Model for Transgressive Sedimentation on the Eastern Shore of Nova Scotia , 1987 .

[21]  John Shaw,et al.  Gravel-barrier migration and overstepping , 1991 .

[22]  G. Fader,et al.  Morphology and seismic stratigraphy of the inner continental shelf off Nova Scotia, Canada: Evidence for a −65 m lowstand between 11,650 and 11,250 C14 yr B.P. , 1994 .

[23]  Garry C. Rogers,et al.  An assessment of the megathrust earthquake potential of the Cascadia subduction zone , 1988 .

[24]  J. Clague,et al.  Late Quaternary sea levels and crustal movements, coastal British Columbia , 1982 .

[25]  T. F. Morris,et al.  Postglacial tectonic and sea level history of the central Canadian Arctic , 1991 .

[26]  W. Peltier,et al.  Ice Age Paleotopography , 1994, Science.

[27]  D. Forbes,et al.  Coastal impacts of climate change: Beaufort Sea erosion study , 1994 .

[28]  J. Barrie,et al.  Post glacial sea levels on the Western Canadian continental shelf: evidence for rapid change, extensive subaerial exposure, and early human habitation , 1995 .

[29]  W. Peltier,et al.  Global Sea Level Rise and the Greenhouse Effect: Might They Be Connected? , 1989, Science.

[30]  D. Forbes Coastal erosion and nearshore profile variability in the southern Beaufort Sea, Ivvavik National Park, Yukon Territory , 1997 .