ECPC’s June 2002 Seasonal Forecasts

 

contributed by J. Roads, S. Chen, J. Ritchie

 

Experimental Climate Prediction Center Scripps Institution of Oceanography UCSD, 0224

La Jolla, CA 92093

 

 


1. ECPC’s Forecast System

 

As previously discussed by Roads et al. (2001a), the Scripps Experimental Climate Prediction Center (ECPC) currently uses the reanalysis I version (Kalnay et al. 1996) of the National Centers for Environmental Prediction’s (NCEP’s) medium range forecast (MRF) model or global spectral model (GSM; Roads et al. 1999). These global forecasts (4xdaily-7 days and weekly to 12-weeks) start from the NCEP operational 00UTC global analysis. The GSM then forces a regional spectral model (RSM; Juang and Kanamitsu, 1994; Juang et al. 1997; Chen et al. 1999, Anderson et al. 2000, Roads and Chen 2000) in order to gain increased spatial resolution (50-25 km resolution) for several selected regions (US, CA, SW, Brazil). At even smaller space (2-km resolution) and time scales (8xdaily to 2 days) either the NCEP analysis or GSM forces a corresponding nonhydrostatic mesoscale spectral model (MSM; Juang, 1997) for the Hawaiian Islands. All atmospheric models are based upon the same physics used in the GSM and can, in principle, be updated as the GSM is updated. Output products from the atmospheric models include a fire weather index (FWI, see Roads et al. 1997) and associated variables such as 2m-temperature, relative humidity and 10m-windspeed as well as precipitation and soil moisture. The global atmospheric model is now forcing an ocean model and corresponding ocean forecasts are discussed in Auad et al. (2002).

 

2. Forecast Skill Evaluations

 

4 years worth of forecasts (208 forecasts) have been used to develop a GSM forecast climatology dependent upon season as well as lag. Both means and standard deviations were derived in order to provide normalized (by the standard deviation) anomalies. As discussed by Roads et al. (2001b,c, d) and Chen et al. (2001), the GSM provides skillful forecasts of temperature, precipitation, soil moisture and a fire weather index at long forecast ranges. Although the greatest skill occurs initially and then decays, daily, weekly or monthly forecast skill does not ever reach zero and forecasts averaged into monthly and seasonal averages demonstrate significant skill (see Reichler and Roads 2002), which may be comparable to empirical long-range forecast methodologies. Similar evaluation efforts are underway for the regional forecasts, which currently use the GSM initial state and boundary conditions, as well as the GSM climatology.

 

3. Global seasonal GSM forecasts and US monthly RSM forecasts

 

Fig.s 1,2,3,4 show the GSM and RSM seasonal forecast anomalies normalized (by GSM standard deviations) of 2-m surface temperature, precipitation, soil moisture and the FWI for June-Aug. 2002.

 

Above normal seasonal temperatures (Fig. 1) are now being forecast for California, Northeast Brazil, Central Africa, Northern Europe and Greenland, central Africa, Asia and the central Pacific, South Atlantic and Indian ocean. Below normal temperatures are being forecast for the North Atlantic and Southern Indian ocean and Argentina as well as the eastern portion of the US.

 

Above normal seasonal precipitation forecasts (Fig. 2) include the eastern US, Central Pacific, southern Europe, central Asia, and Siberia. Below normal precipitation is being forecast for the western US, Venezuela, western equatorial Africa, Russia, and the maritime continent.

 

Soil moisture (Fig. 3) forecasts are indicating that the western US, most of Africa, northern Europe, Australia, Southeast Asia and Venezuela will be dry. Wet regions include the Amazon, Peru, eastern US, and Siberia will be wet. Some, but not all of the dry regions, should be ameliorated by increased precipitation.

 

The seasonal FWI (Fig. 4) strongly corresponds to the soil moisture variations with increased danger over most of the western US, Canada, Venezuela, Central Africa, northern Europe, and China. Decreased danger is expected over the eastern US, Amazon, South Africa, and southern Europe.

 

Other experimental GSM and RSM forecast fields (wind speed, relative humidity) and additional forecast months) can be found at http://ecpc.ucsd.edu/projects/ellfb/. Additional forecast ranges, variables, and regions are displayed at http://ecpc.ucsd.edu/m2s/m2s_ECPC_forecasts.html/. All forecasts and new experimental fire danger (USFS fire danger indices), land surface, and ocean predictions (seasonal to decadal) can be linked from http://ecpc.ucsd.edu/predictions/.

 

References

 

Anderson, B.T., J. O. Roads, S. -C. Chen, and H-M.H. Juang, 2000: Regional Simulation of the Low-level Monsoon Winds Over the Gulf of California and Southwest United States. JGR-Atmospheres, 105 (D14) 17,955-17969.

 

Auad, G., A. Miller, J. Roads 2001: Ocean Forecasts. JGR (submitted)

 

Auad, G., J.O. Roads, A. Miller, and D. Cayan, 2001:  An ocean model response to NCEP, COADS and FSU surface flux fields. Journal of Geophys. Res  (in press).

 

Chen, S. -C., J.O. Roads, H. -M. H. Juang, M. Kanamitsu, Global to regional simulation of California's wintertime precipitation. J. Geophys. Res., 104(24), 31517-31532, 1999.

 

Chen, S-C. J. O. Roads, and M. Wu, 2001: ECPC’s Asia forecasts.  Journal of Terrestrial-Atmosphere-Oceanography, 12, 377-400.

 

Juang, H. -M. H., and M. Kanamitsu, 1994: The NMC nested regional spectral model. Mon. Wea. Rev., 122, 3-26.

 

Juang, H. -M. H., S. -Y. Hong and M. Kanamitsu, 1997: The NCEP regional spectral model: an update. Bulletin Amer. Meteor. Soc., 78, 2125-2143.

 

Kalnay, E. et al., 1996: The NMC/NCAR reanalysis project, Bull. Am. Meteor. Soc., 77, 437- 471.

 

Reichler, T. and J. Roads, 2002: Role of initial and boundary conditions in seasonal predictability. Nonlinear Processes in Geophysics (submitted)

 

Roads, J.O., S. -C. Chen, F. M. Fujioka, H. Juang, and M. Kanamitsu. 1997. Global to Regional Fire Weather Forecasts. Int. Forest Fire News, 33-37.

 

Roads, J.O., S. -C. Chen, M. Kanamitsu, and H. Juang, 1999: Surface Water Characteristics in the NCEP Global Spectral Model and Reanalysis, J. Geophys. Res. 104, 19307-19327.

 

Roads, J.O. and S-C. Chen, 2000:  Surface Water and Energy Budgets in the NCEP Regional Spectral Model. JGR-Atmospheres. 105 (D24), p. 29, 539.

 

Roads, J., S. -C. Chen, J. Ritchie, 2001a: ECPC’s Weekly to Seasonal U.S. Forecasts of FWI, Soil Moisture, and Precipitation. ELLFB bulletin, Dec. 2001.

 

Roads, J.O., S-C. Chen and F. Fujioka, 2001b:  ECPC’s Weekly to Seasonal Global Forecasts. Bull. Amer. Meteor. Soc., 82, 639-658.

 

Roads, J., B. Rockel, E. Raschke, 2001c: Evaluation of ECPC’s Seasonal Forecasts Over the BALTEX Region and Europe. Meteorologische Zeitschrift. (in press).

 

Roads, J. and S. Brenner, 2001d: Global Model Seasonal Forecasts for the Mediterranean Region. Israel Journal of Earth Sciences (in press)



 

 

Fig. 1 Temperature seasonal forecasts normalized (by GSM standard deviation) anomalies: (upper) global forecast; (lower) US forecast.


 

Fig. 2 Precipitation seasonal forecasts normalized (by GSM standard deviation) anomalies: (upper) global forecast; (lower) US forecast.


 

Fig. 3 Soil Moisture seasonal forecasts normalized (by GSM standard deviation) anomalies: (upper) global forecast; (lower) US forecast.


 

 

Fig. 4 FWI seasonal forecasts normalized (by GSM standard deviation) anomalies: (upper) global forecast; (lower) US forecast.