1. Recent Climate Change Modeling Results Eric Salathé Climate Impacts Group University of Washington

2. Global Climate Models 20th Century Validation

3. IPCC Scenarios for Pacific Northwest Climate Change 2-10 ºF 1.6-4.3 ºF 0.7-1.8 ºF

4. Range of Projected Climate Change for the Pacific Northwest from Latest IPCC Climate Simulations

7. 21st Century Change

8. Shift in Pacific Storm Track Salath é, Geophys Res Lett, 2006 Observed 20th Century Model Composite 21st Century Model Composite

9. Downscaling

10. Empirical Downscaling Assumes climate model captures temperature and precipitation trends Quick: Can do many scenarios Shares uncertainties with global models Regional Climate Model Based on MM5 regional weather model Represents regional weather processes May produce local trends not depicted by global models Additional modeling layer adds bias and uncertainty Downscaling Methods Used in CIG Impacts studies

11. Mesoscale Climate Model  Based on MM5 Weather Model  Nested grids 135-45-15 km  Nudging on outermost grid by forcing global model  Advanced land-surface model (NOAH) with interactive deep soil temperature

12. Potential Surprises How does loss of snowpack feed back on the climate? How do changes in the winds affect the local climate? Are their changes in cloudiness that can affect the local rate of warming?

13. MM5 Simulations ECHAM5 global model to force the mesoscale system 1990-2000 to see how well the system is working 2020-2030, 2045-2055, 2090-2100 Climate Change

14. 1990s Validation Obs Record Max Obs Record Min Obs Mean Max Obs Mean Min MM5 Min Day of Year Temperature (°F) 1995 Daily Max and Min Temperature at SeaTac MM5 Max

15. 1990s Validation Gridded ObservationsMM5 - NCEP ReanalysisMM5 - ECHAM5 January July 1990-2000 Mean Surface temperature

16. Evaluation of Future Runs Because there are some biases in the GCM runs, results for future decades (2020s, 2040s, and 2090s) will be evaluated against the ECHAM5-MM5 1990-2000 baseline

17. Winter Warming 1990s to 2050s Temperature Change Difference between MM5 and ECHAM5

18. Loss of Snow cover and Warming Snow Cover ChangeTemperature Change

19. Consistent trend over 21st Century 2020s2050s2090s

20. MM5 Compared to raw Climate model 2020s2050s2090s

21. Spring 1990s to 2050s Temperature Change Difference between MM5 and ECHAM5

22. Pressure gradient and Cloud Pressure ChangeCloud Change

23. Trend over 21st Century 2020s2050s2090s

24. 2020s2050s2090s MM5 Compared to Raw Climate Model

25. Winter Trends at Various Stations MM5 - ECHAM510 IPCC Models

26. Applications: Air Quality

27. Applications: Hydrology

28. Summary  Projected Pacific Northwest Climate Change  warming: 1/4 to 1 ºF/decade  Probably more warming in Summer than Winter  Precipitation changes uncertain – Possibly wetter winters and drier summers  Challenges  Deficiencies in Global model propagate to regional model  Biases from regional model  Mesoscale model simulates different climate signal from global model  Loss of snow amplifies warming in Winter and Spring  Increased cloud cover in Spring -- reduces effect of snow loss