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Pacific Northwest Climate Model Scenarios 2008 Climate Impacts Group & Department of Atmospheric Sciences University of Washington Eric Salathé Philip.

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Presentation on theme: "Pacific Northwest Climate Model Scenarios 2008 Climate Impacts Group & Department of Atmospheric Sciences University of Washington Eric Salathé Philip."— Presentation transcript:

1 Pacific Northwest Climate Model Scenarios 2008 Climate Impacts Group & Department of Atmospheric Sciences University of Washington Eric Salathé Philip Mote Valérie Dulière Emily Jump

2 19 Models From IPCC Fourth Assessment nationalitymodelequilibrium sensitivityTCR BCCRn.a. CCSM32.71.5 CGCM (T47)3.41.9 CGCM (T63)3.4n.a. CNRMn.a.1.6 CSIRO3.11.4 ECHAM53.42.2 ECHO-G3.21.7 FGOALS2.31.2 GFDL-CM2.02.91.6 GFDL-CM2.13.41.5 GISS-AOMn.a. GISS-ER2.71.5 HADCM33.32.0 HADGEM14.41.9 INMCM2.11.6 IPSL4.42.1 MIROC4.02.1 MIROC-hires4.32.6 PCM2.11.3

3 Biases (20th c, minus NCEP)

4 20th century seasonal cycle

5 20th century trend

6 Observed Sea level pressure (NCEP)

7 Model Performance observed

8 Ranked Model Performance

9 Emissions scenarios IPCC Fourth Assessment Global

10 PNW Temperature Change 10°F 0°F

11 Scenario Selection - T/P Scatter

12 2040s - 1980s PNW

13 Projected Temperature temperature2020s2040s (°C)oldnewoldnew lowest0.40.60.80.9 average1.11.2*1.62.0* highest1.81.92.62.9

14 Projected Precipitation precipitation2020s2040s %oldnewoldnew lowest-4-9-4-11 average21*22* highest6129

15 Future Storm Track Changes North America Asia Europe NP Stronger N Atlantic Storm track Stronger N Pacific Storm track ULBRICH ET AL. 2008 Change from 1960-2000 to 2080-2100 Composite of 16 Global Climate Models

16 IPSL ECHAM5 SRES A1BSRES B1 CCSM3 Percentages of change in the annual maximum daily precipitation with a 10 years return period for each grid cell between 1981-2000 and 2046-2065. +12.2% +18.8% +11.4% +10.8% +11.8% +10.6% Projected Future Changes from Climate Models (2046-2065 versus 1981-2000)

17 Global models must be downscaled for regional studies

18 Downscaling -- Winter

19 Downscaling -- Summer

20 Mesoscale Climate Model  Based on Regional Weather Model (MM5, WRF)  Nested grids 135-45-15 km  Advanced land-surface model (NOAH)  Forced by Global Climate Model output (boundary conditions)

21 observed sea level rise 1961-2003 1993-2003 1961-2003 1993-2003

22 Projected global SLR 2090s

23 Local vertical land motion Verdonck (2006) Pacific Northwest Geodetic Array

24 SLR Estimate Components20502100 NW Olympic Peninsula Central & Southern Coast Puget Sound NW Olympic Peninsula Central & Southern Coast Puget Sound Very Low Global SLR9 cm18 cm Atm. Dynamics-1 cm- 2 cm VLM-20 cm- 5cm0 cm- 40 cm-10 cm0 cm Total-12 cm (-5”)3 cm (1”)8 cm (3”)-24 cm (-9”)6 cm (2”)16 cm (6”) Medium Global SLR15 cm34 cm Atm. Dynamics0 cm VLM- 15 cm- 2.5 cm0 cm-30 cm- 5 cm0 cm Total0 cm (0”)12.5 cm (5”)15 cm (6”)4 cm (2”)29 cm (11”)34 cm (13”) Very High Global SLR38 cm93 cm Atm. Dynamics7 cm15 cm VLM-10 cm0 cm10 cm- 20 cm0 cm20 cm Total35 cm (14”)45 cm (18”)55 cm (22”)88 cm (35”)108 cm (43”)128 cm (50”)

25 Summary Temp and precip: central values roughly the same as 2005 estimates 0.5F/decade warming and little change in annual total precip Increased likelihood of drier summers, wetter winters, heavy rains Range of projected temp, precip, sea level: no problem to serious consequences


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