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Uncertainties in Assessing Climate Change Impacts on California’s Water Resources California Water and Environmental Modeling Forum February 25, 2004 Jamie Anderson, Ph.D., P.E. Joint DWR-USBR Climate Change Work Team Rose is Rose Potential Impacts of Climate Change Air temperature Precipitation timing and quantity Sea level rise Runoff timing and quantity What risks does climate change pose for the management of California’s water resources? Climate Change Work Team Francis Chung Jamie Anderson Messele Ejeta Sanjaya Seneviratne Aaron Miller Chris Enright Levi Brekke Ganesh Pandey BG Heiland GOAL Provide qualitative and quantitative estimates of effects of climate change on California’s water resources Provide information that is relevant to water resources decision makers including assessment of risks Risk = f(Hazards, Consequences, Probability) Hazards Climate Change Hazards For this talk, hazards are defined as increments of potential climate change – Air temperature – Precipitation – Sea level rise We are relying on climate modelers to forecast possible future climate conditions, and thus assess the hazards of climate change. Our climate change team currently assesses potential consequences that those climate change scenarios could have on California’s water resources. Future goal: RISK assessments Consequences Floods and Droughts • Rainfall intensity and durations • Frequency and magnitude of floods and droughts Water Supply • Water Demands human and vegetation • Inflows to Reservoirs amount and timing • System Operations size and timing of flood control space; reliability of supplies Water Quality • Drinking WQ • Environmental WQ River and lake temperatures In-stream flow requirements San Francisco Bay-Delta • Levee Stability (flooding or sea level rise) • Sea Water Intrusion Probability Challenge Given the variability and uncertainty in climate projections over California, how do we apply climate change impacts assessment to planning and management of California’s water resources? Climate Change Predictions for Northern California Differ Precipitation Divergence in trend and magnitude Air Temperature Models agree that air temperature increases, but vary in the magnitude and rate of increase (Source: D. Cayan, April 2003,ISAO Workshop) Characterizing Climate Change Uncertainty • Seek advice from other experts • Develop/apply techniques for quantifying the uncertainty in climate change predictions • Bookend approach – A lot warmer and wetter – A little bit warmer and drier • Focus on predictions with least uncertainty – Increase air temperature only – Sea level rise Initial Climate Change Investigations • Bookend approach – A lot warmer and wetter (HadCM2 2010-2039 +1.4°C and +26.4% precip) – A little bit warmer and drier (PCM 2010-2039 +0.4°C and -2.3% precip) • Focus on predictions with least uncertainty – Increase air temperature only (1.5°C, 3°C, 5°C) – Sea level rise • Challenge is to assign probabilities to each scenario, e.g. assume that each bookend or sensitivity range is equally likely Consequence Assessment • Bookend and sensitivity analysis approaches provide ranges of consequences for assumed hazards Delta Inflow wy1922-1994 Bookend Approach 4500 PCM 2010 - 2040 2020 Base Conditions HCM 2010 - 2039 4000 Largest range during winter 3500 -200 TAF in Dec Flow (TAF) 3000 +1,100 TAF in Mar 2500 2000 1500 1000 500 0 OCT NOV DEC JAN FEB MAR APR MAY JUN JUL AUG SEP Delta Inflow wy1922-1994 Sensitivity Analysis 4000 2020 Base Conditions + 3 degrees C + 5 degrees C 3500 Shift in snowmelt and runoff Flow (TAF) 3000 2500 2000 1500 1000 500 0 OCT NOV DEC JAN FEB MAR APR MAY JUN JUL AUG SEP Risk Assessment • The bookend and sensitivity analysis approaches provide ranges of consequences for assumed hazards • Without assuming probabilities for the hazards – Risk assessment has yet to be conducted – Management choices have not been defined • Uncertainty analysis is needed Climate Change Uncertainty Analysis • Develop monthly sensitivity patterns for: – Air temperature – Precipitation – Natural runoff • Watershed scales (e.g. Oroville, Shasta, etc) • Evaluated at projection milestones (e.g. 25 years out, 50 years out) • Account for projection uncertainty: – Patterns from multiple CO2 increase scenarios and/or multiple GCMs of each CO2 scenario Goals of Climate Change Risk Assessment • Determine probabilities and potential impacts of incremental climate change on California’s water resources • Risk information can be used to: – Develop management plans – Determine priorities in resource allocation – Develop mitigation measures • Better information on climate change projection uncertainty is needed to conduct this type of risk assessment