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Multi-instrument Wind Comparisons at Howard University Beltsville campus: An update
B. Demoz1, B. Gentry2, T. Bacha1, K. Vermeesch2,5, H. Chen2,5, D. Venable1, E. Joseph1 G. Koch3, U. Singh3, M Boquet4, L. Sauvage4 1Howard University, 2NASA/GSFC, 3NASA/LaRC 4Leosphere, France, 6SSAI 1
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Wind Lidars: The Howard Experiment Location
Outline: HU-Beltsville Research Campus (HU-BRC): Location, Goals, Instrumentation Wind Lidars: The Howard Experiment: Objective and Instrumentation Results GLOW-Sonde: method + summary GLOW-Profiler(415MHz) VALIDAR-GLOW-ACARS-Sonde Clear sky case and a Cold front case GLOW-VALIDAR merging: Hybrid-Demonstration Lidar Wind retrievals and clouds Summary
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Wind Lidars: The Howard Experiment Location
Semi-urban site Major Pollution corridor Integrate Science and Education Extensive instrumentation Extensive collaboration Dulles Airport National BWI HU Beltsville NASA/GSFC UMBC PSU UMD UVA MDE Major Pollution Transport corridor Beltsville * is located in a region of high population density * is surrounded by many federal, state agencies and universities (NASA, NWS, UMBC, PennState, UVa, UMD, MDE and many others) * is located in a major corridor of air pollution to the north Atlantic * is surrounded by 3-major airports and is under a major air transport corridor
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Wind Lidars: The Howard Experiment: Objective; Instruments
Experiment Goals: NASA 3D-wind concept Compare molecular and aersol-based Doppler wind retrieval Evaluate performance of wind lidars Main Instrumentation: Wind lidars: NASA/GSFC: GLOW NASA/LaRC: VALIDAR Leosphere: WLS70 Wind - Standard: Sonde/RS92/CFH Tower/Sonic ACARS – FAA/NWS 915 Mhz – MDE Profiler A comparison of wind lidar technology is ongoing at the Howard University Beltsville Campus. The goal of the experiment was to compare two of NASA’s state-of-the-art wind lidar technology instruments. The VALIDAR is an aerosol-based lidar system from NASA/LaRC while the GLOW is a molecular-based lidar from NASA/GSFC. This experiment is the first time these two systems have been operated side by side. In addition, the commercial wind lidar from Leosphere, France (the WindCube), a 915 MHz profiler, ACARS winds and different types of radiosondes participated. What is Aircraft Communicating And Rrespons Ssystem? Is an instrument flying on a plane? Yes. Commercial planes have sensors. What is NASA 3D-wind concept? Put together two different wind lidars (based on molec. and aer.) to cover all the altitude range? Yes. Profiling radiometer is the WV one from Stick? ISTP 2009: Delft, Netherlands, October 2009 4
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Wind Lidars: The Howard Experiment: GLOW-VALIDAR-Leosphere ACARS-Profiler-Sonde
Leosphere GLOW VALIDAR Λ: 1.54um 355 nm nm Scope: 15 cm (?) m 15 cm E/Pulse: 25mJ(?) mJ 250 mJ RRate: pps 5 pps SPattern: zenith/15deg. programmable Zenith/45-deg. Principle: aerosol Molecular aerosol (Double-edge) Range: < 2km > 2km < 8km The fig. in the background shows both molec. and aer. Techniques? I don’t remember exactly (even Upendra explained to me once)! If you are at the wings of the line, any change is related to wind. pps=Hz right (pulse per second)? Yes.
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Wind Lidars: The Howard Experiment 11-12 March 2009: A cold front case
GLOW operation continued to present
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Wind Lidars: The Howard Experiment: GLOW-Sonde: Method
Wind variability within sonde flight time needs to be considered GLOW-Sonde: time AND altitude should be considered Note: GLOW scans in a 45degree cone.
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Wind Lidars: The Howard Experiment: GLOW-Sonde
Excellent correlation: Months of data For this example: R2 ~0.9; Slope of ~1.0; Intercept ~ 0.4 Note: at 15km, GLOW wind is averaged over 30km but the correlation holds!
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Wind Lidars: The Howard Experiment GLOW-Profiler: Summary
GLOW profile is 33min. average 2 nearest 15min. profiler data Compute layer averages; nPoints is # of GLOW-profiler pairs Data divided in height bins.
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Wind Lidars: The Howard Experiment ACARS: Analysis Method
reduced 3-hr wind forecast error by 40% (overall improvement of 11%) reduced 12-hr wind forecasts of winds improved by 5% ** Aircraft Communications Addressing and Reporting System (ACARS) Data used within 50km of Beltsville – white (50m); Magenta (30km) AND, within a given averaging time.
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Wind Lidars: The Howard Experiment 11-12 March 2009: A cold front case
Rain VALIDAR Leosphere GLOW NOTE: Relative frontal structure and dynamics is well visualized by all lidars!
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Wind Lidars: The Howard Experiment 11-12 March 2009: A cold front case
Cloud 11 March 2009 RS92: 2223 ● NWS: 2300 ● GLOW: 2316 ● VALIDAR: ● ACARS: ● LEOSPHERE: Note Cold frontal case Sonde-sonde variations Good Performance in rain ACARS variability
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Wind Lidars: The Howard Experiment ACARS-GLOW-VALIDAR-Sonde-WLS70
NOTE: ACARS variability in 1hr GLOW above 10km VALIDAR ~ 10min. Ave. 24 Feb. 2009: NWS sonde: 2300 GLOW (33min;2355, VALIDAR – ACARS:
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Wind Lidars: The Howard Experiment ACARS-GLOW-VALIDAR-Sonde-WLS70
24 Feb. 2009: NWS sonde GLOW - 33min;2355 VALIDAR – ACARS NOTE: ACARS variability (1hr ave.) GLOW above 10km All in good agreement.
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Wind Lidars: The Howard Experiment GLOW-VALIDAR: 24-25 February 2009
VALIDAR: < 6km GLOW: 2-15km Optimum (R2>0.7) 4-5km 24-25 Feb. wind speed
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Wind Lidars: The Howard Experiment GLOW-VALIDAR
24-25 Feb. wind speed 24 Feb 2009: VALIDAR/GLOW/Sonde merged. Profile: 0-15km Res. 3min. Profile is possible
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Wind Lidars: The Howard Experiment GLOW- Cloud effects
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Summary/Conclusion Wind lidars compared to many “standard” instruments. Hybrid DWL Experiment demonstration Cases studies for front, clear-sky, conditions sampled. Cloud effects are being investigated. Data base of lidar wind in various conditions archived
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Wind Lidars: The Howard Experiment IAD Sonde - Reanalysis
What do you plot on upper right? Max speed for month? Yes. I don’t get the diff. bet. The two curves. One is for maximum speed at 12.5km and the other is 10km. To see any variations. The red statements are “requirements” in eneral or achievements by your systems? over the East Coast areas of US (65W-85W, 25N-50N); ECMWF reanalysis ( )
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Wind Lidars: The Howard Experiment: 11-12 March 2009: A cold front case
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