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Photo Credit: Con Desplanque,
Dr. Danika van ProosdijDept. of Geography
Dykelands: Strategic Importance for Climate Change
Adaptation
MCCAP workshop Feb 2013
Outline
Extensive low lying intertidal environments
Dyking history & subsidence
Truro
Moncton
Sackville
Amherst
Wolfville
Windsor
Freshwater flooding
Geographical Setting
• Other areas: Annapolis valley
• predicted relative sea level rise 1.2 – 1.93 m by 2100 (includes increase in tidal amplitude) (Greenberg et al., 2012; Daigle 2011)
• Increased frequency & intensity of storm activity
Consequences of Climate Change
• damage to coastal infrastructure
• increased property loss
• increased flood risks & potential loss of life
• coastal erosion
• freshwater flooding & dam failure
Greenburg et al., 2012• RSLR~0.41 – 0.79 m by 2055 • Risk of storm surge is therefore predicted to increase
Storm Surge• impact depends on tide level
• water level determines duration
• cause floods & are destructive
• SLR will increase storm surge effects
• dykes have either overtopped or breached on numerous occasions
Strategic Importance for Climate Change Adaptation
Source: Webster et al., 2011
• Dykes are the second line of defense after coastal wetlands & no longer simply protect agricultural land
• Over time residential, public and commercial development has taken place on adjacent lands which are now vulnerable to dyke overtopping or breaching.
• Perceived perception of safety
• It is estimated that temporary delays caused by flooding on the TransCanada Hwy between NS and NB will halt more than $50M/day of trade (Webster et al. 2012).
Factors Affecting VulnerabilitySubsidence & isolation from coastal sediment input
• Isolated from tidal flow and new sediment input, the agricultural soils behind the dyke will compact and subside over time.
• Foreshore marsh however continues to receive sediment & increases in elevation
• Results in significant difference in elevation in front & behind dyke
• Net effect = ponding of salt or freshwater flooding & potential blockage (siltation) of aboiteaux structures
• one way • cannot open at high tide• delay FW drainage
Aboiteaux
Truro, NS, March 31, 2003(Photo Claude Barbeau; http://www.novaweather.net/Flood_2003.html)