Circulation, structure and dynamics of a buoyant coastal current' - PowerPoint PPT Presentation

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Circulation, structure and dynamics of a buoyant coastal current'

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Bob Chant, Scott Glenn, Phillip Bogden. American Meteorological Society. Albuquerque New Mexico. January 13-19, 2001. Cold. Warm. Warm. Cold and Salty. Fresh ... – PowerPoint PPT presentation

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Title: Circulation, structure and dynamics of a buoyant coastal current'


1
Circulation, structure and dynamics of a buoyant
coastal current. Bob Chant, Scott Glenn,
Phillip Bogden American Meteorological
Society Albuquerque New Mexico January 13-19,
2001
Cold
2
  • Motivation
  • Characterize Circulation and Dynamics of Coastal
    Current
  • Provides target for numerical modeling
  • Results can be used to assess accuracy of other
    techniques.
  • -Airborne altimetery
  • -Turbulence Sensors
  • -Modeling

3
Buoyant Coastal Current
Warm
Fresh
Warm
Cold and Salty
Cold
4
Towed ADCP/CTD data-July 28, 2000
Along-Shelf (color) and Cross-Shelf
(vectors) Currents.
Salinity (color) and Temperature (contour)
5
. ADCPs at 2,3,4,5 p-sensor T-chain at 2
4
REMUS 2
REMUS 3
REMUS 4
REMUS 5
6
Depth Average Flow
Sectionally Averaged Flow
7
Along-shore flow fluctuations are in geostrophic
balance
8
Sectionally averaged Along-shore
Analyze Flow during Southward Flows V lt -10 cm/s
9
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10
Mean Flow (red) and Stratification (blue) (v lt
-10)
10
Along Shore Flow
-10
10
10
-10
-10
10
4
4
4
4
-4
-4
11
Warm
Fresh
Cold
Cold
12
Cross-Shore Momentum Equations
Depth Averaged
Depth Dependent
13
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14
Conclusions
  • Surface and bottom Ekman layers are evident in
    event-averaged moored ADCP data. However,
    transport in the bottom layer is approximately
    one third of tb/rf.
  • Sectionally averaged fluctuating along-shore
    currents are geostrophically balanced.
  • In the near shore, weak stratification prevents
    bottom-stress from penetrating the entire water
    column. Mixing coefficients are strongest in the
    bottom mixed layer (10-2 m2/s), weakest in the
    interior (510-4 m2/s) and of intermediate values
    towards the surface (10-3 m2/s)
  • Fluctuating depth averaged and near bottom
    currents are highly
  • constrained by bathymetry. Surface currents are
    constrained by the coastline only within an
    internal Rossby radius from the coast.

15
20 cm/s 0.5 dyne/cm2
16
Principle Components of fluctuating
currents Surface-red Bottom-Blue Depth
Average-Black
17
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18
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19
Record Mean Flow
fu
tb/rH
Residual
ts/rH
10 cm/s
20
Surface Stress is Red Bottom Stress is Blue
Along-Shelf Stress
tbgtts (despite tb underestimate)
Cross-Shelf Stress
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