Airborne Doppler lidar surface returns: data products other than tropospheric winds G. D. Emmitt and...
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Transcript of Airborne Doppler lidar surface returns: data products other than tropospheric winds G. D. Emmitt and...
Airborne Doppler lidar surface returns: data products other than
tropospheric winds
G. D. Emmitt and C. O’HandleySimpson Weather Associates
Charlottesville, VA.
Hangzhou, China
October, 2002
TODWL: the program(Twin Otter Doppler Wind Lidar)
• SPAWAR and ONR 35/SBIR Program provided the lidar and supported its integration into the CIRPAS Twin Otter
• IPO has co-funded the lidar adaptation to the Twin Otter.
• IPO has solely funded the mission planning, flight hours, data collection and the post flight installation of the lidar in a trailer for inter-flight research.
TODWL : the aircraft
• Navy Twin Otter operated by CIRPAS out of Marina, CA
• Unpressurized (~ 10 ft normal operations)• Cruise speeds 100 - 140 kts• Equiped with:
– GPS/INS– Dropsonde– aerosol probes– temperature, water vapor, turbulence sensors
TODWL : the instrument
• 2µm coherent detection• 4-6 mJ (330 nsec pulse)• 80 Hz• water cooled• ~7-10% total system efficiency• 10 cm two axis scanner, side door mounted• GUI with realtime instrument control and data display• Weight: 250lb Power: 1.5 KW
TODWL 2-axis scanner
The Experiments
• Airborne missions over various water bodies (open ocean, surf zone, large rivers, lakes and wetlands) in the vicinity of Monterey, CA
• Laboratory studies using a water slide to simulate observations at differing incidence angles
Objectives
• Check out the operations of an airborne 2µm coherent, semi-hemispherical scanned DWL
• Investigate the utility of water surface returns at 2µm for space-based and airborne DWLs (ocean, lake, river, & wetlands)
• Compare DWL wind soundings with RAOBs, microwave sounders, met towers, ground-based DWLs and assorted surface observations
• Investigate the use of an airborne DWL to provide cal/val data for scatterometers and RadarSat
• Demonstrate the application of LAHDSSA for future space-based DWL missions.
• Collect aerosol data along with lidar data to assist in the interpretation of signals from the LAS
TODWL soundinglooking up (20seconds)
TODWL soundinglooking down (20 seconds)
Microwave soundingFt Ord (30 minutes)
0030 UTC March 2002
Aircraft flight level
Water surface returns as a function of incidence angle at 2µm with a coherent Doppler
lidar
Modeled reflectance from ocean surface for a wind speed of 7.5m/s (Tratt, 2002)
along wind direction
Cross wind direction
200
400
600
1000
800
1200
1400
1600
Ran
ge f
rom
air
craf
t (m
eter
s)
LAS returns
Water surface returns
Nadir angle
Relative spectral amplitude (range corrected)
using 400 shot integration
TODWL returns collected over Monterey Bay, 12 March 2002
Single shot data used to obtain 400 shot averageat ~3 degrees off nadir
Water surface
Single shot data used to obtain 400 shot averageat ~33 degrees off nadir
Water surface
400 shot integrated signal
saturations
TODWL signal as a function of nadir angle
Spectrum for range gate 20 associated with the data shown in previous slide. The data has notbeen fully corrected for the aircraft forward motion
WaterLAS
Observing ocean wave motion and the atmospheric
Layer Adjacent to the Surface (LAS)
Monterey Bay12 March 2002
Nadir view over water
0 100 200 300
ALO N G -TR A C K D ISTA N C E (M )
0
40
80
120
160
200S
IGN
AL
AM
PL
ITU
DE
- 1
0
1
2
VL
OS
(M
/S)
R H I N AD IR SC A NW ATER SU R FA C E VLO S (D ASH ED R ED )W ATER SU R FA C E S IG N AL AM PLITU D E (BLAC K)R U N N IN G A VG O VER 41 SH O TS (30 M )
TRO U G H
CR ESTCR EST
Investigation of Organized Large Eddies
within the Marine Atmospheric Boundary Layer
Summary
In addition to horizontal and vertical winds, an airborneDoppler lidar can be used to study water surface motionsand their correlations with aerosols. These correlationshave significance in the interpretation of data obtainedwith space based lidars and also the parameterizationof fluxes over water surfaces at wind speeds above thosethat produce whitecaps. The investigation of Organized Large Eddies will be among the objectives of futureTODWL flights
Acknowledgements
• This work was funded by the Office of Naval Research through the Center for Interdisciplinary Remotely-piloted Aircraft Studies and by the Integrated Program Office of NPOESS
TODWLTwin Otter Doppler Wind Lidar
Funded by USN and IPO
First Flight Series11-15 Feb. 2002
2 m lidar10 cm scanner(1st of its kind)
Navy Twin OtterOperated by
CIRPAS
Equipped for aerosolsampling
VADS to measureLOS component ofaircraft TAS
Signals 5 km aheadof aircraft for backscatter calibration using particleprobes
PIs: Emmitt and Bluth
TODWL obtaining a wind profile above the aircraft
CTI
Particle Probe Cluster
Cloud Streets over Monterey Bay, February, 2002
TODWL: participants
Simpson Weather Associates (SWA)
G. D. Emmitt ([email protected]) Science lead
C. O’Handley ([email protected]) Data processing and advanced algorithm development
S. Greco ([email protected]) Ancillary data from sounders, buoys, numerical models and other data sources for comparison
Center for Interdisciplinary Remotely Piloted Aircraft Studies (CIRPAS)
R. Bluth ([email protected]) Platform lead
Nava Roy ([email protected]) Software support
Haf Jonsson ([email protected]) Aerosol probe data responsibility
Mike Duncan ([email protected]) Project oversight
Roy Woods ([email protected]) Pilot and aircraft systems engineer
Mike Hubbell ([email protected]) Chief pilot
Coherent Technologies Incorporated (CTI)
Steve Shertz ([email protected]) TODWL would not have happened without his technical support
Phil Gatt ([email protected]) Project responsibility within CTI. Also provided experience based input to the operations of the TODWL lidar
Rod Munson ([email protected]) Software support.
University of Alabama at Huntsville (UAH)
David Bowdle ([email protected]) Aerosol/Lidar backscatter
University of Washington (UW)
Ralph Foster ([email protected]) Arranged for RADARSAT data collection over the Monterey Bay during TODWL flights.
Robert Brown ([email protected]) Involved in the interpretation of QuikScat and RADARSAT data taken during TODWL under-flights
United States Geological Survey (USGS)
John Costa ([email protected]) Arranged for surface flow velocity observations on the San Joaquin River during TODWL overflights.
NOAA Environmental Technology Laboratory (ETL)
M. Hardesty ([email protected]) Helped arrange for lidar operations during TODWL over flights
A. Brewer ([email protected]) Operated NOAA’s lidars during the overflights
TODWL Data Inventory and Experiment Summary Series 1 (February, 2002) Date Experiments Time(PST) Other Data Comments 2/09/02 Ground based
checkout 1102 – 1138 None Checking on pointing
directions relative to aircraft.
2/11/02 Engineering checkout flight
1700 – 1751 None Not well documented for analysis
02/13/02 Under flights of RADARSAT and QuikScat; Ocean surface returns; Aircraft attitude checks; Backscatter runs using different view angles
0630 - 0915 RADARSAT QuikScat FT.Ord Microwave Buoy data Eta Model fields GOES images
Saw cloud streets over bay; Ocean waves with small areas of whitecaps; several transects of shoreline near Ft. Ord.
02/14/02 Lake, river and canal over flights; flight above marine strat.
1445 - 1815 USGS Observations of surface velocity on San Joaquin River
Focus of flight was on the river surface observations. Flight legs at 6500 ft provided opportunities to take down VADS, nadir (up and down) stares, and cloud reflectivity observations
02/15/02 Dropsonde comparisons and VADS over land and water
1325 - 1500 Ft. Ord microwave; Buoys Dropsondes(2)
The two dropsondes were deployed from 6500 ft and were dropped through a cloud layer.
Series 2 (March, 2002) Date Experiments Time (PST) Other Data Comments 03/12/02 Long transects of Bay
to get variety of water reflectance data and wind profiles; Comaprison with Ft Ord microwave; Lidar and probe data comparisons.
1430 – 1638 Ft Ord Sounder CODAR?? Accelerometer Probes
Best set of data for water reflectance from different angles. Also good data for up and down VADS. Also good data fro probe comparisons
03/13/02 Trip from Monterey to Boulder via Las Vegas.
1010 - 1735 Probes Had to limit operations below 12000ft to protect hard drives. Most of flight was at 17000ft. Very strong winds near Las Vegas..dust storm
03/14/02 Grounded due to icing conditions
1227 –1238 BAO Took some raster scans while sitting on ramp. Interesting wind structures seen.
03/15/02 Overflights of ground based lidars, BAO tower and Platteville microwave sounder
0928 – 1116 (LST)
CTI lidars NOAA lidars BAO tower Platteville Microwave sounder Probes
Overflights at 10500 scanning down; overflights at 6500 scanning up. Lots of snow returns during down VADS.
Returns over Monterey Bay during 1 second
LAS returns
Water returns