GEOSCAN, résultats de la recherche


TitreHalifax Harbour extreme water levels in the context of climate change: scenarios for a 100-year planning horizon
AuteurForbes, D L; Manson, G K; Charles, J; Thompson, K R; Taylor, R B
SourceCommission géologique du Canada, Dossier public 6346, 2009, 26 pages,
Documentdossier public
Mediaen ligne; numérique
Lat/Long OENS-63.7500 -63.4500 44.7500 44.5000
Sujetsniveaux d'eau; changements du niveau de la mer; variations du niveau de la mer; inondations; potentiel d'inondation; techniques de cartographie; Changement climatique; géologie de l'environnement; géologie marine
Illustrationsphotographs; location maps; plots; graphs; aerial photographs
Bibliothèque de Ressources naturelles Canada - Ottawa (Sciences de la Terre)
ProgrammeRenforcement de la résilience des communautées canadiennes face aux changements climatiques, Géosciences de changements climatiques
Diffusé2009 11 19
Résumé(disponible en anglais seulement)
A Halifax Harbour Plan is being developed within the context of the 25-year Regional Municipal Planning Strategy in the Halifax region of Nova Scotia. This strategy recognizes the importance of climate change and the need for a precautionary approach to minimize negative impacts of rising sea level. Airborne LiDAR data were acquired in 2007 to produce a high-resolution digital elevation model (DEM) as a basis for mapping flood limits. The selection of flood levels for adaptation planning required an understanding of present and future sea-level rise (SLR), vertical land motion, extreme water levels (combined tide and surge), harbour seiche and wave runup. Relative sea level in Halifax Harbour has risen at 3.2±0.13 mm/a since 1920 through a combination of regional subsidence (1.6±0.3 mm/a) and local SLR (~1.6 mm/a). Scenarios of future extreme water levels were developed using (1) current local SLR, (2) the upper limit of the 2007 IPCC projections, and (3) a higher projection based on a growing scientific consensus that the IPCC upper limit may have been overly conservative. These projections of SLR (0.16, 0.59, and 1.3 m over ~100 years) were combined with regional subsidence and extreme water levels for 2-, 10-, and 50-year events derived from a generalized extreme values distribution of annual extreme water levels in Halifax Harbour. The resulting water levels were applied to the LiDAR DEM to visualise the extent and depth of flooding for each event. A plausible upper limit with very low probability was developed by superimposing the record storm surge on the highest tide with a sea-level rise of 1.3 m. A buffer ranging from 1 to 2 m was considered to account for observed values of seiche and wave runup in various parts of the harbour. This study provides the scientific basis for a set of plausible scenarios for a 100-year planning horizon, but the choice of water level for planning purposes is a policy decision.