By Sebastian Weissenberger, Omer Chouinard
The ebook offers a concise and interdisciplinary outlook at the affects of weather swap on coastal components and the way coastal groups adapt to them. the 1st bankruptcy analyses how sea point upward thrust, altering ocean stipulations, or elevated weather variability and the socio-environmental context of the coastal quarter ends up in weak groups. the second one bankruptcy addresses variation techniques and instruments, and provides a few examples in their program around the globe. The 3rd bankruptcy describes participative motion study initiatives undertaken in New Brunswick and the way this group dependent procedure has enabled groups to extend their weather resilience.
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Additional resources for Adaptation to Climate Change and Sea Level Rise: The Case Study of Coastal Communities in New Brunswick, Canada
Ice-sheet and sea-level changes. Science, 310, 456–460. Antonov, J. , & Boyer, T. P. (2005). Thermosteric sea level rise 1955–2003. Geophysical Research Letters, 32, L12602. 1029/2005GL023112. Arendt, A. , Echelmeyer, K. , Harrison, W. , Lingle, C. , & Valentine, V. B. (2002). Rapid wastage of Alaska glaciers and their contribution to rising sea level. Science, 297, 382–386. Benoît, H. , Gagné, J. , & Bourassa, M. N. (2012). Rapport sur l’état des océans pour la zone de gestion intégrée du golfe du Saint-Laurent (GIGSL) (vol.
Where resilience breaks down. The notion of «tipping points» has been applied to the Earth-climate system by Lenton et al. (2008). In a dynamic system, not only the amplitude and duration but also the timing of perturbations is important to assess their criticality. In the context of climate change, gradually shifting baselines, such as increasing ocean temperatures and acidity or accelerating coastal erosion lower the threshold for critical perturbation over time. In the case of extreme weather events, the frequency of events is important to consider, in addition to their amplitude.
Journal of Invertebrate Pathology, 106, 71–78. , & White, N. (2006). A 20th century acceleration in global sea-level rise. Geophysical Research Letters, 33, L01602. Clark, R. , Fox, C. , & Livermore, M. (2003). North Sea cod and climate change— modelling the effects of temperature on population dynamics. Global Change Biology, 9, 1669–1680. , & Marshall, S. J. (2000). Substantial contribution to sea-level rise during the last interglacial from the Greenland ice sheet. Nature, 404, 591–594. Daigle, R.