Pacific Northwest MM5 Weather Forecasts: Information
For a description of our experimental WRF forecasts click here
General Information: The Department of Atmospheric
Sciences at the University of Washington is now running the Penn State/NCAR
mesoscale model version 3.7.3 (MM5 v3.7.3) twice a day in order to produce
high resolution meteorological forecasts for the Pacific
Northwest. This effort, supported by a consortium of local, state, and
federal agencies, has several goals:
- To provide high resolution meteorological fields for air quality
applications, weather forecasting, and other needs.
- To test the viability of local numerical weather forecasting
completed on relatively low-cost workstations.
- To provide a large number of mesoscale model forecasts to
determine model strengths, weaknesses, and biases.
- To improve mesoscale model physics and data assimilation
approaches.
- To test the potential of directly coupling an atmospheric forecast
model to air quality and hydrological numerical models.
Change Log: For the latest information on our setup, please
consult the Change Log for Pacific Northwest MM5 Numerical Forecasts
Model Configuration: The MM5 numerical forecasts currently feature
an outer grid of 36 km horizontal resolution that covers much of western
North America and the northeastern Pacific, a nested grid of 12 km resolution
that covers Washington, Oregon, Idaho, western Montana, southern
British Columbia, and northern sections of California, Nevada, and
Utah and an inner 4 km resolution grid encompassing all
of Washington and Oregon plus the western third of Idaho. The regions
covered by each domain, showing topography and land use categories are
shown in these plots:
A land use category color key is included in the links above, you may
view it alone here.
A detailed description of the domain boundaries as well as the
actual terrain.namelist are given here. Detailed land use
information for each domain was derived from the 1-km USGS digital
database, with some subjective modification using other data sources.
The model utilizes 38 vertical full-sigma levels see below, and is run in
non-hydrostatic mode in order to limit pressure gradient force errors
over the complex terrain. An upper-radiative boundary condition is used
to allow gravity waves to radiate through the model top without being
reflected. The following table describes the phyics options we are
currently using:
Phyics Options:
| Physics | Comments |
| CCM2 Radiation |
We changed the effective ice radius as used in radcsw.F from the
default 14.6 microns to 35 microns. We are using ICLOUD=1, using
resolved clouds. |
| Reisner 2 Moist Physics | Includes graupel. |
| Kain-Fritsch Cumulus |
As of 5 August 2004, we are using this on all domains. |
| MRF PBL | Also known as the Hong-Pan PBL (Hong and Pan
1996). |
| 5-layer Soil Model |
Dudhia scheme predicting temperature
at approximately 1, 2, 4, 8, and 16 layers with a fixed substrate
below. |
| Bucket Soil Model (IMOIAV=2) |
Used on all domains, with 36-km and
12-km domains initialized with 20-km RUC values of soil moisture.
Begun with 2004081900 forecast. Note: As released, the MM5
code does not allow IMOIAV=2 and IFSNOW=1 at the same time; thus, we
turn off IFSNOW with this option. (See also comparison.) |
Here are the exact mmlif files that are used to run the model: 36/12 km mmlif and 4 km mmlif (these
two links are updated with each model run.). NOTE: EXTFRQ and EICER
are U.W. modifications and will not work with standard MM5 versions.
For more information on any of these options, see the MM5 chapter of
the
MM5 tutorial notes.
Initializations: Currently two model runs are performed.
One utilizes initial and lateral boundary conditions for
the MM5 that are generated by interpolation of the National Centers
for Environmental Prediction (NCEP) "ETA" model analysis and
forecast fields. This MM5-ETA run only includes the 36 and 12 km domains.
The second initialization uses NCEP's GFS model (formerly known as AVN or
MRF) at 1-degree lat/lon resolution for nearly all fields. The
exceptions are: 1) SST is from the 1/4 degree OTIS grids, 2) surface
temperature is from the ETA 221 grids (40-km grid spacing), and 3)
subsurface soil temperature and moisture are also from ETA 221 grids.
Forecast: Forecasts are computed as follows:
- MM5-ETA: 24 processor SUN Microsystems Ultra Enterprise 6500 Server
For increased speed, the SUN MM5 code is parallelized using Kuck &
Associates' OpenMP compiler,
Guide.
- MM5-GFS: a 40-processor HP Xeon Beowolf cluster running Debian
Linux.
Currently, the model is run for a 72 hour forecast period over the 36 and
12 km domains and up to 48 hours for the inner 4 km domain. The
MM5-ETA finishes in roughly 3.0 hours of wallclock time, while the
MM5-GFS finishes in roughly 4.5 hours of wallclock time.
Future Improvements: The modeling system is constantly being
improved. Among the changes we hope to make in the near future are:
- Improve initial analysis through reanalyses of eta initialization fields
using regional surface, upper-air, and wind profiler observations.
- Incorporate four-dimensional data assimilation by means of nudging
the model during a 12-h pre-forecast spin-up period.
Full Vertical Sigma Levels
Sigma: 1.00, 0.995*, 0.99, 0.985*, 0.98, 0.97, 0.96, 0.95*,
0.94, 0.93*, 0.92, 0.91*, 0.90,
0.88, 0.86, 0.83, 0.80, 0.77, 0.74, 0.71,
0.68, 0.64, 0.60, 0.56, 0.52, 0.48, 0.44, 0.40,
0.36, 0.32, 0.28, 0.24, 0.20, 0.16, 0.12, 0.08, 0.04, 0.
* = added 7/9/2001
Half-Sigma Levels
| K-index | Sigma | K-index | Sigma | K-index | Sigma |
| 1 | 0.02 | 2 | 0.06 | 3 | 0.10 |
| 4 | 0.14 | 5 | 0.18 | 6 | 0.22 |
| 7 | 0.26 | 8 | 0.30 | 9 | 0.34 |
| 10 | 0.38 | 11 | 0.42 | 12 | 0.46 |
| 13 | 0.50 | 14 | 0.54 | 15 | 0.58 |
| 16 | 0.62 | 17 | 0.66 | 18 | 0.695 |
| 19 | 0.725 | 20 | 0.755 | 21 | 0.785 |
| 22 | 0.815 | 23 | 0.845 | 24 | 0.87 |
| 25 | 0.89 | 26 | 0.905 | 27 | 0.915 |
| 28 | 0.925 | 29 | 0.935 | 30 | 0.945 |
| 31 | 0.955 | 32 | 0.965 | 33 | 0.975 |
| 34 | 0.9825 | 35 | 0.9875 | 36 | 0.9925 |
| 37 | 0.9975 |
Past Domain Configurations: This table provides all the
necessary information about previous domain configurations.
Questions and Comments: We're always interested
in feedback. Please direct any questions and comments you have to Mark
Albright (marka@atmos.washington.edu) or Cliff Mass (cliff@atmos.washington.edu).