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The LAPS hot start Initializing mesoscale forecast models with active cloud and precipitation proces

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High-resolution grids. Robust data ingest, QC, and fusion. Develop a flexible solution for ... Comparison of parallel model runs using three kinds of initialization (hot, warm, ... – PowerPoint PPT presentation

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Title: The LAPS hot start Initializing mesoscale forecast models with active cloud and precipitation proces


1
The LAPS hot startInitializing mesoscale
forecast models with active cloud and
precipitation processes
  • Paul Schultz
  • NOAA Forecast Systems Laboratory
  • Local Analysis and Prediction Branch

2
Developers of the LAPS hot-start techniques
  • John McGinley, branch chief, variational methods
  • Paul Schultz, project manager, modeler
  • Brent Shaw, modeler
  • Steve Albers, cloud analysis, temp/wind analysis
  • Dan Birkenheuer, humidity analysis
  • John Smart, everything

3
Goals
  • Address NWP spin up problem
  • Explicit short-range (0-6 h) QPFs and cloud
    forecasts
  • Focus on a local modeling capability
  • Must be computationally inexpensive
  • Exploit all locally-available meteorological data
  • High-resolution grids
  • Robust data ingest, QC, and fusion
  • Develop a flexible solution for easy technology
    transfer
  • Hardware/OS independence
  • Choice of mesoscale model

4
LAPS II Three-Dimensional Cloud Analysis
METAR
METAR
METAR
5
Cloud typing
Cumulus vertical motions
6
LAPS II Dynamic Balance Adjustment
( ) b are background quantities () are
solution increments from background ( ) are
observation differences from background
7
LAPS II Dynamic Balance Adjustment
FH FL
8
Example first forecast hour, 5-min frames
hot start loop
9
First real-time implementation
  • Real-time diabatically initialized MM5 runs since
    Fall 2000
  • MM5v3-4 with minor modifications
  • 125 x 105 x 34 domain, 10-km grid spacing
  • K-F cumulus parameterization
  • Schultz explicit microphysics
  • Four 24-h forecasts per day with hourly output
  • Displayed on AWIPS (FSL and BOU NWS) and WWW
  • http//laps.fsl.noaa.gov/cgi/laps_fcst_products.cg
    i
  • Typically available 1.5 h after cycle time

10
Quantitative Assessment
  • Comparison of parallel model runs using three
    kinds of initialization (hot, warm, cold)
    otherwise identical
  • Objective verification of model performance using
    hot start vs. other initialization methods
  • Approximately 40 forecast cycles during Jan 2001
  • Gridded comparisons using LAPS analysis as truth
  • Computed various threat scores, RMSE, etc.

11
Model Initialization Comparisons
Time-n Time
Cold start
MM5 Forecast
no LAPS analysis interpolate from larger-scale
model
Eta
Warm start
LAPS Analyses
pre-forecast nudging to a series of LAPS
analyses sometimes called dynamic initialization
MM5 Nudging
MM5 Forecast
Hot start
MM5 Forecast
diabatic initialization using the balanced LAPS
analysis
LAPS II
Dynamically balanced, Cloud-consistent LAPS
Eta LBC for all runs
12
Results of Initialization Comparisons
13
Results of Initialization Comparison
14
Summary of first results
  • Software is very reliable
  • Hot start works well for winter precipitation
    systems
  • Several forecast-hours of added value
  • What about summertime?
  • Verification not complete
  • Encouraging cases
  • Some known problems

15
Example 21 June 2001/0600 UTC Run
MM5 00 hr Forecast, Valid 21/0600 UTC
GOES IRNOWRAD, Valid 21/0600 UTC
16
Example 21 June 2001/0600 UTC Run
MM5 01 hr Forecast, Valid 21/0700 UTC
GOES IRNOWRAD, Valid 21/0700 UTC
17
Example 21 June 2001/0600 UTC Run
MM5 02 hr Forecast, Valid 21/0800 UTC
GOES IRNOWRAD, Valid 21/0800 UTC
18
Example 21 June 2001/0600 UTC Run
MM5 03 hr Forecast, Valid 21/0900 UTC
GOES IRNOWRAD, Valid 21/0900 UTC
19
Example 21 June 2001/0600 UTC Run
MM5 04 hr Forecast, Valid 21/1000 UTC
GOES IRNOWRAD, Valid 21/1000 UTC
20
Example 21 June 2001/0600 UTC Run
MM5 05 hr Forecast, Valid 21/1100 UTC
GOES IRNOWRAD, Valid 21/1100 UTC
21
Convection -- the next problem
  • 10-km grid is too coarse except for biggest
    storms
  • too fine for conventional convective
    parameterizations
  • storms start late, produce excessive precip
  • subgrid-size cumuli alias to resolvable scale
  • 4 km? 3 km?
  • Improvements will come, QPF bias will persist
  • Parameterization for subgrid cumuli probably
    required down to 250 m
  • Real life get a computer, configure the model,
    solve problems as they arise

22
Intriguing aspects of the D/FW TMU project
  • Texas mesonet
  • surface obs in every country
  • wind profilers
  • CRAFT project
  • real-time access to full-volume, full-resolution
    WSR-88D radars
  • Internet II (Abilene)
  • Includes Lubbock, D/FW, but nothing south of that
    yet
  • Local or remote implementation?

23
Related Presentations at NWP conference
  • Dynamic Balance
  • WAF/NWP P1.11, McGinley and Smart
  • Cloud Analysis
  • WAF/NWP JP2.5A, Schultz and Albers
  • Operational Evaluation/Case Studies
  • WAF/NWP 3.9, Shaw et al.
  • WAF/NWP P2.3, Birkenheuer et al.
  • MP P4.21, Szoke and Shaw

Available in pdf format from laps.fsl.noaa.gov
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