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Development of the Regional Arctic Climate System Model (RACM) --- Department of Civil and Environmental Engineering University of Washington May, 2010.

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Presentation on theme: "Development of the Regional Arctic Climate System Model (RACM) --- Department of Civil and Environmental Engineering University of Washington May, 2010."— Presentation transcript:

1 Development of the Regional Arctic Climate System Model (RACM) --- Department of Civil and Environmental Engineering University of Washington May, 2010 Performance of the VIC land surface model in coupled and uncoupled simulations

2 Current Status The macroscale hydrology model VIC has been successfully coupled with WRF through CCSM4 flux coupler CPL7. WRF/VIC successfully runs more than 6 months over Arctic in wr50a grid with ocean and sea ice as a data model. Currently WRF/VIC is basically ready for long-time (multi-year) simulation since VIC has restart function and also is able to produce its own output.

3 Simultations WRF-VIC : WRF/VIC coupled simulation over the Arctic region in the wr50a grid (Jan. – Jun. 2003) with ocean and sea ice conditions prescribed (“data model”). Initial and boundary conditions are from FNL. VIC-obs: VIC Offline Simulations of the Arctic domain (1990-2003) at 50km resolution driven by meteorological observation (provided by Xiaogang Shi). WRF-noah: Original WRF simulation (by Joan Cassano’s group over wr50a grid driven by NCEP- 2 reanalysis data(Sep. 2000 - ). WRF2: Original WRF simulation (by JuanXiong He ) over wr50a grid driven by FNL (Jan. 1 - 15 2003 ). SST

4 Modeling Framework Arctic Domain wr50a resolution runs: Jan. – June. 2003 Configuration WV (WRF/VIC) Features specific to Cold- Land Processes: Two-layer energy balance snow model (Storck et al. 1999) Frozen soil/permafrost algorithm (Cherkauer et al. 1999, 2003) Lakes and wetlands model (Bowling et al. 2004) Blowing snow algorithm (Bowling et al. 2004)

5 Validation of coupled WRF/VIC modeling system WRF/VIC Precipitation JFM 2003 AMJ 2003 Observation WRF/VIC produces drier climate especially over Russia, Finland, Sweden and Norway.

6 Validation of coupled WRF/VIC modeling system WRF/VICObservation JFM 2003 AMJ 2003 WRF/VIC basically captures temperature pattern but has significantly cold bias over Russia.

7 VIC offline simulation ------ VIC in coupled environment

8 Surface Runoff JFM AMJ WRF/VICVIC-ObsNCEP-2

9 Snow Water Equivalent Field JFM AMJ WRF/VICVIC-ObsNCEP-2

10 Latent Heat JFM AMJ WRF/VICVIC-ObsNCEP-2

11 Sensible Heat JFM AMJ WRF/VICVIC-ObsNCEP-2

12 Surface Skin Temperature JFM AMJ WRF/VICVIC-ObsNCEP-2

13 First Layer Soil Temperature JFM AMJ WRF/VICVIC-ObsNCEP-2

14 WRF/VIC ------ WRF-noah

15 Precipitation --- WRF-VICWRF-noah WRF2 JFM AMJ WRF-VIC Jan. 1-15

16 Surface Air Temperature --- WRF-VIC WRF-noah WRF2 JFM AMJ WRF-VIC Jan. 1-15

17 Surface Runoff --- WRF-VICWRF-noah

18 Snow Water Equivalent Field---- WRF-VIC WRF-noah WRF2 WRF-VIC Jan. 1-15 JFM AMJ

19 Latent Heat --- WRF-VICWRF-noah

20 Sensible Heat --- WRF-VICWRF-noah

21 Surface Skin Temperature --- WRF-VICWRF-noahWRF2

22 First Layer Soil Temperature WRF-VICWRF-noahWRF2

23 Parrellizing VIC land model in CCSM system to improve computing performance. Implement VIC routing model into RACM Rout surface and subsurface runoff into rivers Future Work Performing multi-year simulation to evaluate the model performance


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