Ý Notes
Slide Show
Outline
1
BroadBand ADCP Basics 3
  • Discussion of Concepts
  • re
  • How It Works
2
Autocovariance Function
  • Decorrelation Effects
3
Autocovariance Function
  • Water speed: Uwater = C/2 x p / (Df x Tapart )
  • p is determined from autocovariance function (acvf) of echo time series for each depth cell
    • ACVF tells the average delay and similarity between recurring patterns in a time series
    • ACVF outputs correlation
      • Measure of similarity between recurring patterns
      • Says how well you detect and measure pulse separation
  • Key point
    • Low correlation => poor estimate of water velocity
      • i.e., sd (p) varies inversely with correlation
4
Information In Acvf
  • Water speed: Uwater= C/2 x p / (Df x Tapart )
  • p = N x carrier cycles + fraction of cycle
  • (1) (2)
  • Complex autocovariance function has 2 types of information
    • Magnitude (correlation): used to measure (1)
    • Phase information: used to measure (2)
  • Key point
    • Phase values are only reliable if correlation is high
    • Poor correlation results in noisy (or none) water velocity measurements
5
Velocity and Correlation
  • Water speed: Uwater= C/2 x p / (Df x Tapart )
  • p = N x carrier cycles + fraction of cycle
  • (1) (2)
  • Standard deviation of Uwater = sd (Uwater)
    • sd (Uwater) = C/2 x 1/ (Df x Tapart ) x sd (p )
  • Factors affecting sd (p )
    • Part (1) .. *quantizing* noise (N±1)
    • Parts (1), (2) .. correlation between 1st, 2nd pulses
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Decorrelation Effects
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Decorrelation Effects
  • ACVF => measures AVERAGE delay and similarity between patterns recurring in a time series
  • Poor correlation => due to TOO MUCH VARIABILITY in the delay or similarity between these patterns over the duration of time series
  • Consider separately 2 aspects of too much variability
    • Delay between pulses
    • Similarity between pulses
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Varying Inter-pulse Delay (Figure)
  • Too much variability in the delay between pulses
    • Blurs 2nd pulse and its average location when ACVF is computed for each depth cell
    • Result: Low correlation
      => noisy or no velocity
  • Causes
    • High Shear: velocity changes too much across the depth of the bin (notably the ambiguity resolving bin)
    • Beam divergence: differences between velocity measured at edges of beams greater at higher speed
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Velocity Shear Effect Figure
  • Velocity profile vs. Pulse Separation in Echo


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Velocity Shear In Bin Figure
  • Velocity shear vs. Pulse Separation in Echo


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Beam Divergence Effect Figure
  • Beam Width vs. Pulse Separation in Echo


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Action: Inter-pulse Delay
  • Options to improve correlation
    • Smaller bins .. Reduce range of velocities in cell
    • Slow down .. Reduce range between Doppler shifts measured at beam edges
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Rapidly Varying Scatterers
  • Too much variability in the similarity between pulses
    • Back-scattering sources change too fast before the 2nd pulse arrives
    • Degrades the *signature* of 2nd pulse compared with 1st pulse
    • Result: Low correlation => noisy or no velocity
  • Causes
    • Turbulence and Boat Heave: scatterers move rapidly between bins (or along beam)
    • High boat speed, Pitch and Roll: scatterers move rapidly across beam (short residence time)
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Rapidly Varying Scatterers Figure
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Action: Varying Scatterers
  • Options to improve correlation
    • Slow down .. Scatterers move across beam slower
    • Use larger bins .. fractional change in scatterers is less
    • Increase ambiguity velocity (reduce inter-pulse delay at transmit) .. 2nd pulse arrives sooner after 1st pulse sees more of same scatterers
    • Move measurement section to place with smoother bottom or calmer surface .. Vertical water motions are reduced
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BroadBand ADCP Basics 3
  • Discussion of Concepts
  • re
  • How It Works