Haida Gwaii – Summary table for climate impacts, projected changes and sectoral impacts
Climate Impact | Projected Changes | Evidence Quality | Sectoral Impacts | Impacts Summary | Evidence Quality |
---|---|---|---|---|---|
Air Temperature | Average air temperatures may increase by 1.4°C (0.8°C to 2.2°C) by 2050 and 2.2°C (1.1°C to 3.5°C) by 2080 [1], [2]; South Haida Gwaii: Average air temperatures may reach ~7.5°C with low emission scenario (RCP 2.6) and ~11.5°C with high emission scenario (RCP 8.5) by 2091-2100 [3]; North Haida Gwaii: Average air temperatures may reach ~8.5°C with low emission scenario (RCP 2.6) and ~12°C with high emission scenario (RCP 8.5) by 2091-2100 [3]; Growing degree days: +317 (+182 to +506) by 2050 and +514 (+264 to +855) by 2080 [1]; Frost free days: +22 (+13 to +31) by 2050 and +32 (+18 to +46) by 2080 [1]; Increases in winter minimum temperatures by 4–9°C by 2080 and summer maximum temperatures by 3–4°C [4]. | High | Threats to: Potential positive benefits to tourism due to warmer and longer summer season [2]. | High | |
Precipitation | Increases in average annual precipitation by 7% (0% to 10%) by 2050 and 9% (4% to 17%) by 2080, and ~10% decrease in summer [1], [2]; Decreasing winter snowfall by -35% (-54% to -11%) by 2050 and -48% (-72% to -22%) by 2080 [1]; South Haida Gwaii: Increasing average precipitation by ~18% (low emissions, RCP 2.6) and ~25% (high emissions, RCP 8.5) by 2091-2100 compared to 1961-1990 baseline [3]; North Haida Gwaii: Increasing average precipitation by ~20% (low emissions, RCP 2.6) and ~22% (high emissions, RCP 8.5) by 2091-2100 compared to 1961-1990 baseline [3]. | High | Potential damaging impacts on ecosystems and habitats [2]; Changes in access and seasonality of traditional foods [2]. | High | |
Sea Level Rise | Extreme low projections of 0.1-0.31m, mean projections of 0.25-0.46m, extreme high projections of 0.95-1.16m [5]; Average sea level may increase by 0.7-1.32m. North and northwest coast may experience ~1.32m, northeast and the southwest coast may experience ~1-1.2m [6]. | Medium | Threats to: Ecological, economic, social and technological impacts and adaptation challenges [8]. | Medium | |
Sea Surface Temperature | South Haida Gwaii: Average sea surface temperature to be ~11.75°C with RCP 2.6 and ~14°C with RCP 8.5 by 2091-2100 compared to 1961-1990 baseline [3]; Increasing sea surface temperature by up to 1.5°C in less than 100 years5; or by ~2.1°C compared to 1995-2008 baseline [9]; average temperature to be ~10.5-12.5°C by 2065-2078 [9]. | High | Potential positive benefits to seagrasses and the kelp species Macrocystisspp [5]; Impacts on a variety of marine species [5]. | + | High |
Ocean Acidification | Decreasing ocean pH levels. South Haida Gwaii: Average ~7.96 ph unit with RCP 2.6 and ~7.69 ph unit with RCP 8.5 by 2091-2100 compared to 1961-1990 baseline [3]. | High | Threats to: Economic impacts on communities due to impacts on aquaculture and potential impacts on fisheries [5], [8]. | Medium | |
Oxygenation | Declining ocean oxygen levels [9]. | High | Impacts on: | High | |
Streamflow | Changing timing of streamflow - earlier freshet, less snowpack, higher water volume earlier in spring [8]. | Low | Threats on salmon migration, spawning, and incubation [8]. | Low | |
Sea Surface Salinity | South Haida Gwaii: Decreasing sea surface salinity by ~1% with RCP 2.6 and ~3.4% with RCP 8.5 by 2091-2100 compared to 1961-1990 baseline [3]; Decreasing sea surface salinity by less than 1% (~0.3 decrease in psu unit) by 2065-2078 compared to 1995-2008 baseline [9], ~5% decrease in sea surface salinity (~1.2 decrease in psu unit) around Masset Inlet [9]. | High | Impacts on: | High | |
Winds, Waves and Storms | Stronger future storm events [2], [10] and increases in storm surge frequency [2]. | High | Threats to: | High | |
General | Increasing intensity of cumulative climate change impacts [5]. | High | Threats to: Northward shift in species range and abundance [12]. | High |
Ecosystems | Communities | Fisheries and Aquaculture | Marine Infrastructure |
* Data specific to MaPP region
α Unless indicated, all sectoral impacts are negative
- PCIC, Plan2Adapt: Summary of Climate Change for Skeena-Queen Charlotte 2050s & 2080s, Pacific Climate Impacts Consortium. https://pacificclimate.org/analysis-tools/plan2adapt (Accessed December 1, 2017).
- PCIC, Climate summary for West Coast Region, Pacific Climate Impacts Consortium, Victoria, BC, 2013. https://www.pacificclimate.org/sites/default/files/publications/Climate_Summary-West_Coast.pdf
- [IPCC WG5]. Canadian Centre for Climate Modelling and Analysis, Environment Canada, 2013. https://www.canada.ca/en/environment-climate-change/services/climate-change/science-research-data/modeling-projections-analysis/centre-modelling-analysis.html
- D.L. Spittlehouse, Climate Change, Impacts and Adaptation Scenarios: Climate Change and Forest and Range Management in British Columbia, British Columbia Ministry of Forests and Range Forest Scienc, 2008.
- T.A. Okey, H.M. Alidina, V. Lo, S. Jessen, Effects of climate change on Canada’s Pacific marine ecosystems: a summary of scientific knowledge, Rev Fish Biol Fisheries. 24 (2014) 519–559. doi:10.1007/s11160-014-9342-1.
- J.M. Kershner, R.M. Gregg, K. Feifel, Climate Change Vulnerability Maps for the North Pacific Coast of British Columbia: Implications for Coastal and Marine Spatial Planning, EcoAdapt, Bainbridge Island, WA, 2014.
- D.S. Abeysirigunawardena, I.J. Walker, Sea level responses to climatic variability and change in northern British Columbia, Atmosphere-Ocean. 46 (2008) 277–296. doi:10.3137/ao.460301.
- MaPP, Climate Change Commitments from MaPP Sub-Regional Marine Plans and the Regional Action Framework (RAF), Marine Plan Partnership, 2016.
- M.G.G. Foreman, W. Callendar, D. Masson, J. Morrison, I. Fine, A Model Simulation of Future Oceanic Conditions along the British Columbia Continental Shelf. Part II: Results and Analyses, Atmosphere-Ocean. 52 (2014) 20–38. doi:10.1080/07055900.2013.873014.
- I.J. Walker, J.V. Barrie, Geomorphology and sea-level rise on one of Canada’s most sensitive coasts: Northeast Graham Island, British Columbia, Journal of Coastal Research, Special Issue. 39:1 (2006) 220–226. doi:10.2307/25741565.
- I.J. Walker, R. Sydneysmith, British Columbia, in: D.S. Lemmen, F.J. Warren, J. Lacroix, E. Bush (Eds.), From Impacts to Adaptation Canada in a Changing Climate, 2008: pp. 1–58.
- L.V. Weatherdon, Y. Ota, M.C. Jones, D.A. Close, W.W.L. Cheung, Projected Scenarios for Coastal First Nations’ Fisheries Catch Potential under Climate Change: Management Challenges and Opportunities, PLoS ONE. 11 (2016) e0145285.