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Modeling Hydrological Impacts of Climate Change The San Pedro Basin Study Case. Aleix Serrat-Capdevila, Juan B Valdes, Javier Gonzalez, Kate Baird , Luis J. Mata, Thomas Maddock III. Regional Precipitation Estimates. GCM Models. MF Recharge. ET. Local Recharge. Data “ Adaptation ”
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Modeling Hydrological Impacts of Climate ChangeThe San Pedro Basin Study Case Aleix Serrat-Capdevila, Juan B Valdes, Javier Gonzalez, Kate Baird, Luis J. Mata, Thomas Maddock III
Regional Precipitation Estimates GCM Models MF Recharge ET Local Recharge Data “Adaptation” Downscaling Alluvial Recharge GW Hydrologic Model Methods
17 Global Climate Models: Mean & 4 extreme modelswettest, driest, hottest, coldest (*) (WM-95, ECH-395, CERF-98, CCSR-96) . (*) Using the regional mean. GCMs and Scenarios • 4 Emission Scenarios: • IPCC Special Report on Emissions Scenarios: A1 MES, A2 MES, B1 MES, B2 MES.
Temperature projections: Scenarios A1 &A2 73.4 F 70 F 65 F
Temperature projections: Scenarios B1 &B2 70.7 F 68 F 65 F
From RAIN to RECHARGEUsing Anderson (1992): Experimental Regression Method For each of the 4 scenarios
Regional Precipitation Estimates GCM Models MF Recharge ET Local Recharge Data “Adaptation” Downscaling Alluvial Recharge GW Hydrologic Model Methods
Yearly estimates 5x5 deg. latlong 1/8x1/8 deg. latlong
Evolution of mean Annual Precipitation (2000-2100)Scenario A1MES, Mean GCM projection
Key questions: • How is climate change affecting SEASONAL and SPATIAL patterns ? • How can we quantify/model these changes ? • Key needs: • Accurate methods to quantify seasonal recharge • Inclusion of temperature effects on evapotranspiration • Compare effects with different basins (regimes)
Evolution of mean Annual Precipitation (2000-2100)Scenario A1MES, driest model CCSR96