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1
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2
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- The profile is composed of a series of 3-d vectors uniformly spaced
through the depths reached by acoustic signals emitted by the ADCP.
- The following slides describe the geometric relationship between the Velocity
Profile and the depths where backscattering sources produce the acoustic
echoes.
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3
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- (1) Transmit Time
- (2) Blank Time
- (3) Time Record of Echoes
- (4) Range Gates
- (5) Measured Depth Layers
- (6) Depth Cells
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4
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5
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- An intermediate step is that Transmit duration is set by the Range Gate
duration. As we will see, the Range Gate time slots in the echo record
are set by the Depth Cell size.
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6
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- After the ADCP transmits, a brief pause or blank in the record is
required to allow acoustic transients or ringing (like a bell) to
dissipate.
- Any echoes recorded during this ring-down period are contaminated by
these transients that are unrelated to the water in motion (i.e.,
Doppler shift = 0).
- Any Doppler shifts computed with such contaminated acoustic data will be
biased low.
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7
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- These time slots
(1) are associated with specific layers in the water column
- (2) record echoes originating from their assigned layers
- (3) sample the center of their layer most and top & bottom least
- (4) overlap with adjacent depth layers, resulting in some mutual
information in successive Range Gates.
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8
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9
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10
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- Most of the echoes heard by a Range Gate, however, originate from the
region within the Depth Cell (due to the spatial-weighting described in
the last slide).
- As a result, data reported for a Depth Cell are predominantly affected
by those depths mapped by the cell.
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11
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12
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- The result is assigned to the associated Depth Cell.
- Although adjoining Depth Cells do not overlap, their associated Range
Gates share some mutual information.
- Successive velocities in the Velocity Profile are therefore slightly
correlated.
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