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1
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- Discussion of Concepts
- re
- How It Works
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2
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- Broader bandwidth => Better results
- Method Differences
- 2-pulse Signal
- Velocity Precision
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3
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- RDI's ADCPs use patented broadband technology.
- Advantages of broadband signaling are everywhere in our daily lives:
better quality, clearer reception, and faster results.
- Examples include high-speed internet access, cable TV, FM stereo radio,
3G cell telephones, GPS positioning, and CD music recordings.
- Improved performance is due to broadband signaling providing more
information.
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4
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- How does broader bandwidth signal =>
more precise / repeatable results?
- Bandwidth: rate at which modulate carrier signal (e.g., by phase shift)
- Determines how many samples are taken by a single acoustic transmission
(*ping*)
- More bandwidth => More independent samples => More information
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5
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- How does broader bandwidth signal =>
more precise / repeatable results?
- More information produces better data set-- better basis, more
confidence for making important decisions
- How is it better?
- ÝIf you wait the same time, you
obtain better certainty of the measurement (signal is clearer)
=> More precise / repeatable results
- You don't have to wait as long to see the signal, so your time series
or boat path have better definition
=> Better resolution in time or space (or both)
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6
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7
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- Bandwidth = sampling rate
- Broadband method
- Broad bandwidth signal => 100's samples per ping
- Noise NOT hide the signal
- Take only few pings
- NO WAITING to see signal
- Narrowband method
- Narrow bandwidth signal => few samples per ping
- Noise can hide the signal
- Must take many pings to reduce noise
- Wait to see signal
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8
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- Broadband method = More information
- More information: top-to-bottom without sacrificing resolution in time,
along boat path OR
- More information in time history, along boat path without sacrificing
resolution top-to-bottom
- Narrowband method
- Trade Off for Improving Data Resolution
- ÝIf you want MORE information in
profile,
COST = LESS information in time history, along boat path
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9
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10
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- Transmit 2 pulses at known time separation: Tapart
- They travel along a beam, away from ADCP
- Suspended material is moving along beam, to ADCP
- At encounter with 1st pulse, an echo is scattered back to ADCP
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11
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12
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- Speed of scatterer = moving with the water = Uwater
- In the time = Tapart , scatterer moves a distance = L
- The 2nd pulse has a round trip shorter by about
- Ý2 x L compared with the 1st
pulse
- So 2nd pulse travels for less time than 1st pulse
- Key Result: in echoes, time between pulses is reduced
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13
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- Speed of pulses = speed of sound = C
- Change in time between pulses in echoes = t
- t = 2 x L / C = 2 x Uwater x Tapart / C
- This gives the water speed
- Ý Uwater= C/2 x t / Tapart
- Key points
- By determining t in the echo data, you know water speed
- Velocity comes from displacement of scatterer during a known time
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14
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15
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- Measurement: Uwater= C/2 x t / Tapart
- Standard deviation of Uwater = sd (Uwater)
- sd (Uwater) = C/2 x 1/ Tapart x sd ( t )
- Key point
- Larger Tapart => smaller sd (Uwater)
- Modes 5, 11 are quieter than Mode 1
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16
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- Estimating velocity from position data
- Compute the change in position with time
- Velocity = (X2 - X1) / elapsed time
- Uncertainty of velocity estimate
- = sqrt(2) x (uncertainty in position) / TIME
- Longer TIME delay between two position fixes
- => more certainty of velocity
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17
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- Discussion of Concepts
- re
- How It Works
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