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Climate change and adaptive human migration Dr. Robert McLeman Department of Geography University of Ottawa
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Theoretical & conceptual backdrop Migration is but one way by which households may adapt to climate-related stress Is not simple stimulus-response process Household adaptation options and migration decisions are condition by access to capital McLeman and Smit 2006
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Empirical work Highlights from 3 projects
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Project 1: Migration vs. other household adaptation options Oklahoma 1930s Severe droughts, crop failures McLeman 2006, 2007 McLeman et al 2007
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Levels of adaptation Actor/scale Governance/ institutions Individual farm Type of adaptation Technological improvements Programs/subsidies Modify farming practices Non-farming adaptations after Smit and Skinner 2002
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1930s Oklahoma droughts Actor/scale Governance/ institutions Individual farm Type of adaptation Technological improvements Programs/subsidies Modify farming practices Non-farming adaptations came too late too costly already at maximum
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1930s Oklahoma droughts Adaptation options constrained by access to economic, social, cultural capital Particular types of capital facilitated out- migration by young, skilled families Feedback effects on adaptive capacity Drought areas lost human capital, social cohesion McLeman et al 2007
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Project 2: Demographic change and community adaptive capacity www.addington.uottawa.ca
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Observed climatic changes in Addington Highlands Shorter, milder winters with less snow Earlier spring conditions Warmer summers with less variability Increasingly windy with occasional micro- bursts (short, high-intensity windstorms)
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Demographic change Population = 2,500 Absolute numbers unchanged from 1901 But…
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Demographic change Population = 2,500 Absolute numbers unchanged from 1901 But…
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Impacts on adaptive capacity Risks Pressure on health & emergency services Fewer people with survival skills Social cohesion breaking down Opportunity Skills of newcomers untapped
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Project 3: Modeling climate- migration Building GIS model to combine climate & demographic data to identify “hotspots’ Start with western Canada – drought- related migration known to have occurred Can we model to local scale areas where severe drought & population decline coincided? McLeman et al. submitted
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Datasets Canada census data 1926, 1931, 1936 Historical climate model data at 10km 2 grid cells (McKenny et al. 2006) Summer monthly temperature and precipitation data selected for 1926-36 Organized according to cumulative frequency of relatively hot, dry conditions
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Population change 1931-36
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Average summer precipitation 1926-36
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Average summer temperatures 1926-1936
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Combined data sets, 1931-36
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Population decline exceeding 10% 1931-36
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Thanks! Dr. Robert McLeman Assistant Professor Department of Geography University of Ottawa Canada K1N 6N5 rmcleman@uottawa.ca
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