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University of Washington Modeling Infrastructure Available for Olympex

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Title: University of Washington Modeling Infrastructure Available for Olympex


1
University of Washington Modeling Infrastructure
Available for Olympex
  • Cliff Mass
  • University of Washington

2
GoalsThe Local Modeling Effort at the UW
  • Provide high-resolution forecasts for mission
    planning.
  • Provide high-resolution simulations to drive
    hydrological modeling
  • Assimilate a wide-range of mesoscale and synoptic
    observational assets to produce the best possible
    description of the mesoscale structures over the
    region.

3
GoalsThe Local Modeling Effort at the UW
  • Evaluate model fidelity, particularly for cloud
    and precipitation fields. Work with partners to
    improve microphysics and other model
    deficiencies.
  • Demonstrate the value of combining the model with
    observations to produce skillful snowpack and
    water-related fields.

4
Important Points
  • The Olympex area offers substantial precipitation
    and terrain ideal for a GPM testbed.
  • Terrain offers the potential to place assets in
    crucial locations, with certainty that you will
    catch the cloud/precipitation structures you
    want.
  • Models are very good in the dynamics of
    orographic flows, so you can get the winds right
    fairly easily.
  • Then you can tear the microphysics/PBL physics
    apart to find the flaws and fix them.
  • Rivers offer a wonderful integration of moist
    processes, both on a short-term and long-term
    basis.

5
NW Modeling Resources
  • High-resolution WRF ARW forecasts at 36, 12, 4,
    and 1.3 km grid spacing completed twice a day.
  • High-resolution (4-km) WRF-DART Ensemble Kalman
    Filter (EnKF) data assimilation system run on a
    three-hour cycle, with intermittent 24-h
    forecasts.
  • 12-km mesoscale ensemble system based on the
    initializations and forecasts of major modeling
    centers.
  • Collection of all real-time data assets over the
    region.

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Optimized Physics for the Region
  • Based on testing hundreds of physics
    combinations, domains, and numerical options.
  • Best performance plus reliability
  • Physics
  • SAS Convection on 4, 12, and 36 km
  • YSU PBL
  • Thompson Microphysics
  • RRTM IR, RRTMG solar radiation
  • NOAH LSM
  • MODIS land use

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MODIS Land Use
15
Regional Data Assimilation and Forecasting
16
EnKF System
  • Based on a large (64 member) ensemble of
    forecasts at 36 and 4 km grid spacing. WRF model
    and DART Ensemble Kalman Filter (EnKF) System
  • Every three hours assimilate a wide range of
    observations to create 64 different analyses.
  • Then we forecast forward for 3 hours and then
    assimilate new observations.
  • Thus, we have a continuous cycle of probabilistic
    analyses.

17
EnKF Ensemble Forecasting System
  • We can run ensemble of forecasts forward to give
    us probabilistic forecasts for any period we
    want. Now doing 24h ahead, four times a day.

18
Improvement in short-term forecast using our
local assimilation system
19
WRF 4 km at same time
20
NWS NAM
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There is Room for Improvement
  • Using the data from the IMPROVE-2 experiment, UW,
    NCAR, Stony Brook and others put a lot of effort
    in improving moist physics.
  • In general, we do an excellent job on the
    windward side of barriers but often overpredict
    in the lee.
  • Probably a microphysical explanation, but PBL
    problems could also be involved.
  • OLYMPEX will provide a comprehensive data set for
    the next round of improvements of model moist
    physics.

24
Small-Scale Spatial Gradients in Climatological
Precipitation on the Olympic Peninsula Alison M.
Anders, Gerard H. Roe, Dale R. Durran, and
Justin R. Minder Journal of Hydrometeorology
Volume 8, Issue 5 (October 2007) pp. 10681081
25
Annual Climatologies of MM5 4-km domain
26
2011-2012
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2012-2013
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Verification of Small-Scale Orographic Effects
31
Dungen
Buck
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Cascade Cumulative Precipitation
West LIne
East LIne
34
Work for the Next Year
  • Provide model data sets to Jessica Lundquist and
    colleagues to test ability to determine snowpack
    from model output.
  • Improve model precipitation/cloud physics
  • Intensive model verification year. Use gauges,
    snow measurement, and hydrological verification
  • Enhance local data assimilation to include all
    regional radars and additional observational
    assets (e.g., TAMBAR aircraft).

35
The End
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