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Expected Impacts of Climate Change on Biome Stability in the Namakwa District : new biome envelope predictions & identification of areas supporting resilience. Dr Stephen Holness & Prof Guy Midgley Springbok March 2012. Components. “Areas of biome stability”
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Expected Impacts of Climate Change on Biome Stability in the Namakwa District:new biome envelope predictions & identification of areas supporting resilience Dr Stephen Holness & Prof Guy Midgley Springbok March 2012
Components • “Areas of biome stability” • Particular parts of the Namakwa District are at higher risk from climate change induced impacts • “Areas important for supporting ecosystem resilience to climate change impacts” • Intact ecosystems have the potential to reduce climate change impacts through supporting ecosystem based adaptation • Particular parts of the district are of particularly high value for supporting cc resilience
Technical process (1) • Revised climate data from 15 GCMs were used to calculate anomalies between now and mid century • Does not focus on a single model • Used the range of predicted outcomes from these models to define three scenarios: • High risk scenarios with low rainfall and high temperatures • a medium risk scenario • and low risk scenario with high rainfall and smallest temperature • Anomaly calculated and combined with current agro hydrology data
Technical Process (2) • MAXENT - widely used ecological modelling and forecasting program (we will now extend this to other methods) • Model of current biomes & test prediction ability • Develop biome maps for future high, medium and low risk scenarios • Identify areas with high risk of biome envelope change and areas which are likely to remain stable.
Can we predict biomes? “Actual current” “Modelled current” • MAXENT models of each biome • Biome determined by strongest model outputs at each site • 86% accurate prediction – most missed blocks have a mixture or are on boundaries
Current Biomes Current Biomes