Title: Satellite Data as used in the Local Analysis and Prediction System LAPS
1Satellite Data as used in the Local Analysis and
Prediction System (LAPS)
- Steve Albers
- May 13, 2008
2LAPS cloud analysis
METAR
METAR
METAR
33D Cloud Image
4Cloud / Radar W-E X-sect
5 Cloud Analysis Flow Chart
6Cloud/precip cross section
7Precip type and snow cover
8Cloud/Satellite Analysis Topics
- 11 micron IR
- 3.9 micron data
- Improving visible with terrain albedo database
- CO2-Slicing method (Cloud-top pressure)
911 micron imagery
- T(11u) best detects mid-high level clouds
- Cloud Clearing Step
- Cloud Building Step
- Iterative Adjustment Step
- Forward model converts cloud-sounding T(11u)
estimate - Constrained 1DVAR iteration fits cloud layers to
observed T(11u)
103.9 micron imagery
- T(3.9u) T(11u) detects stratus at night
- Currently used with 11u cloud-tops for cloud
building - Testing underway for cloud-clearing
- Additional criteria include T(11u) and land
fraction - T(3.9u) T(11u) detects clouds in the daytime?
- Visible may be similar in cloud masking
properties - Visible may be easier for obtaining a cloud
fraction - Cloud Phase?
- Could work using T(3.9u) T(11u) at night
- Cloud-top phase needs blending throughout LWC/ICE
column
11Visible Satellite
- Improving visible with terrain albedo database
- Cloud-clearing (done with current analysis)
- Cloud-building (now being tested)
- Easiest to do over low-latitude oceans
- Accurate sfc albedo can work with VIS 11 micron
cloud-tops - Visible cloud fraction can be used to correct
apparent brightness temperature to yield improved
cloud-top temperature
12Visible Satellite Impact
13CO2 Slicing Method (cloud-top P)
- Subset of NESDIS Cloud-Top Pressure data
- CO2 (fractional) measurements add value
- 11u measurements (0 or 1 cloud fraction)
redundant with imagery? - Imagery has better spatial and temporal
resolution? - Treat as a cloud sounding similar to METARs and
PIREPs
14Temperature Analysis
- Derived Satellite Soundings
- GOES
- POES (via MADIS)
15Wind Analysis
- Cloud Drift Winds (via MADIS)
- 3 hourly
- Experimental 1 hourly
16fdfdfd
GOES/POES Soundings
Cloud-Drift Winds
ACARS Temperature
ACARS/Radar Wind
17Humidity Analysis
- GOES Retrieved Integrated Water Vapor (GVAP)
- Utilizes Gradients
- Tech Memo and Posters by Dan Birkenheuer
- Earlier method uses GOES sounder with OPTRAN
18(No Transcript)
19MM5 Fcst Synthetic Imagery
Implemented by Brent Shaw
20WRF Fcst Synthetic Imagery
- Ongoing with Isidora Jankov and Louie Grasso
(CIRA) - Future efforts incorporating Community Radiative
Transfer Model (CRTM)?
21Going Global with G-LAPS
- Global LAPS Domain running in real-time
- Expanding our satellite image coverage
- global geosynchronous satellites
22Global IR Satellite Animations for Science On A
Sphere (SOS)
- Start with AWC / McIDAS animation
- Apply QC
- Overlay MTSAT imagery supplied by Taiwan CWB
- Merge with Blue Marble using variable
transparency
23Global Cylindrical IR image for SOS
24Global IR Satellite Animations for Science On A
Sphere (SOS)
- Testing with GSD / McIDAS feed
- 15 minute frames
- time interpolation from 30 minute data
- testing with Meteosat Second Generation
25Further Information
26Questions??
27CloudSchematic
28Selected references
- Albers, S., 1995 The LAPS wind analysis. Wea.
and Forecasting, 10, 342-352. - Albers, S., J. McGinley, D. Birkenheuer, and J.
Smart, 1996 The Local Analysis and prediction
System (LAPS) Analyses of clouds, precipitation
and temperature. Wea. and Forecasting, 11,
273-287. - Birkenheuer, D., B.L. Shaw, S. Albers, E. Szoke,
2001 Evaluation of local-scale forecasts for
severe weather of July 20, 2000. Preprints, 14th
Conf on Numerical Wea. Prediction, Ft.
Lauderdale, FL, Amer. Meteor. Soc. - Cram, J.M.,Albers, S., and D. Devenyi, 1996
Application of a Two-Dimensional Variational
Scheme to a Meso-beta scale wind analysis.
Preprints, 15th Conf on Wea. Analysis and
Forecasting, Norfolk, VA, Amer. Meteor. Soc. - McGinley, J., S. Albers, D. Birkenheuer, B. Shaw,
and P. Schultz, 2000 The LAPS water in all
phases analysis the approach and impacts on
numerical prediction. Presented at the 5th
International Symposium on Tropospheric
Profiling, Adelaide, Australia. - Schultz, P. and S. Albers, 2001 The use of
three-dimensional analyses of cloud attributes
for diabatic initialization of mesoscale models.
Preprints, 14th Conf on Numerical Wea.
Prediction, Ft. Lauderdale, FL, Amer. Meteor. Soc.
29Derived products flow chart
30Future Precip analysis efforts
- Combine radar with other data sources
- Model First Guess
- Rain Gauges
- Satellite Precip Estimates (e.g. GOES/TRMM)
31Future LAPS analysis work
- Surface obs QC
- Operational use of Kalman filter (with time-space
conversion) - Handling of surface stations with known bias
- Improved use of radar data for AWIPS
- Multiple radars
- Wide-band full volume scans
- Use of Doppler velocities
- Obtain observation increments just outside of
domain - Implies software restructuring
- Add SST to surface analysis
- Stability indices
- Wet bulb zero, K index, total totals, Showalter,
LCL (AWIPS) - LI/CAPE/CIN with different parcels in boundary
layer - new (SPC) method for computing storm motions
feeding to helicity determination - More-generalized vertical coordinate?
32Recent analysis improvements
- More generalized 2-D/3-D successive correction
algorithm - Utilized on 3-D wind/temperature, most surface
fields - Helps with clustered data having varying error
characteristics - More efficient for numerous observations
- Tested with SMS
- Gridded analyses feed into variational balancing
package - Cloud/Radar analysis
- Mixture of 2D (NEXRAD/NOWRAD low-level) and 3D
(wide-band volume radar) - Missing radar data vs no echo handling
- Horizontal radar interpolation between radials
- Improved use of model first guess RH cloud
liq/ice
33Cloud type diagnosis
Cloud type is derived as a function of
temperature and stability
34LAPS data ingest strategy
35Dummy Image
36Humidity Analysis