NonContact Velocity Measurements on Simulated River Surfaces Using Coherent Doppler Lidar Preliminar - PowerPoint PPT Presentation

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NonContact Velocity Measurements on Simulated River Surfaces Using Coherent Doppler Lidar Preliminar

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Title: NonContact Velocity Measurements on Simulated River Surfaces Using Coherent Doppler Lidar Preliminar


1
Non-Contact Velocity Measurementson Simulated
River Surfaces Using Coherent Doppler
LidarPreliminary 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_at_msfc.nasa.gov David.Bowdle_at_msf
c.nasa.gov
2
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

3
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
4
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

5
(Very) Preliminary Experiment at MSFC
Target
350 m range
Target
Lidar
Lidar
6
Water Slide Geometry
Slit
Water Flow
Lidar Beam
Water slide
Nadir Angle
7
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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14
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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