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MSFC/GHCC 1 2 micron pulsed ground based lidar Non-Contact Velocity Measurements on Simulated River Surfaces Using Coherent Doppler Lidar Preliminary Results Prepared by J. Rothermel* and S.C. Johnson (NASA MSFC) P.A. Kromis (Computer Science Corporation) Earth Science Department NASA Marshall Space Flight Center Updated by D. Bowdle** (University of Alabama in Huntsville) *jeffry.rothermel@msfc.nasa.gov*jeffry.rothermel@msfc.nasa.gov**David.Bowdle@msfc.nasa.gov
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MSFC/GHCC 2 2 micron pulsed ground based lidar MSFC Coherent Doppler Wind Lidar Initiated April 1999 Purpose: CDWL technology validation Atmospheric properties research Space CDWL concepts investigation CDWL targets research Student Instruction Location: MSFC Building 4467 GSFC van (proposed) Van or trailer (future) Aircraft (future) Initial components: Transceiver, 50 mJ, 6.6 Hz, 2.017 microns, FL pumped 10 cm telescope from Schwartz Electro-Optics, Inc. Full hemispheric scanner (Bldg. 4467) Data acquisition & processing
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MSFC/GHCC 3 2 micron pulsed ground based lidar Long-term Objective Streamflow Measurement with Doppler Lidar Complement proposed microwave radar measurements Relationship among surface velocity profile, bottom topography, and discharge Based on phased approach Controlled experimental conditions (initial phase) Collaborations with USGS, U. Washington (later phases) Doppler lidar is only technique that can directly measure the influence of near-surface winds
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MSFC/GHCC 4 2 micron pulsed ground based lidar Background Water surface velocity measurements depend on: Lidar wavelength Surface roughness Incidence (or nadir) angle Turbidity Surface contaminants (e.g., foam) Depth of penetration (of order millimeters at 2 micron) Near-surface wind velocity
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MSFC/GHCC 5 2 micron pulsed ground based lidar Target Target Lidar Lidar ~350 m range (Very) Preliminary Experiment at MSFC
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MSFC/GHCC 6 2 micron pulsed ground based lidar Water Slide Geometry Water slide Nadir Angle Slit Water Flow Lidar Beam
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MSFC/GHCC 7 2 micron pulsed ground based lidar Experiment Parameters MSFC Doppler lidar, 6.6 Hz, 2.017 m Velocities toward lidar are negative (-) Water discharge nozzles: weirgate on new waterslide Water slide surface composition: plexiglass Lidar beam footprint: ~10 cm Discharge depth: several mm (variable) Nadir angles at target: 30, 60 deg Integration: 20 pulses Range gate, velocity plots: 210 m, centered on target Range gate, range plots: 38.4 meters Range to target: ~350 meters Minimum range: ~150 meters Number of good range gates in air near target: ~5
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MSFC/GHCC 8 2 micron pulsed ground based lidar
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MSFC/GHCC 9 2 micron pulsed ground based lidar
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MSFC/GHCC 10 2 micron pulsed ground based lidar
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MSFC/GHCC 11 2 micron pulsed ground based lidar
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MSFC/GHCC 12 2 micron pulsed ground based lidar
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MSFC/GHCC 13 2 micron pulsed ground based lidar
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MSFC/GHCC 14 2 micron pulsed ground based lidar Conclusions and Plans Conclusions Velocity standard deviation for hard target is ~0.1 m/s. Velocity decreases slowly as reservoir empties, allows integration Surface tension effects from untreated plexiglass slide surface create flow channeling, with variable water layer thickness non-riverine water surface microstructure Sanding the plexiglass surface reduces surface tension effects virtually eliminates flow channeling nearly mirror smooth water surfaces Plans Resume lidar operations (after minor repairs) Test runs with variable flow velocity and layer thickness Test runs with controlled surface condition
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