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Comparison

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Geostrophic currents along transects and Dynamic Height. Anomaly at levels ... Geostrophic velocity at upper surface between stations. adp = dF = -gdz ... – PowerPoint PPT presentation

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Title: Comparison


1
Comparison of Calculated Geostrophic
Currents and ADCP data and Observation of
Features in Leg II
LT Rodrigo Obino OC3570 Final Project
2
Objectives
  • Use of temperature, calculated salinity and
    pressure
  • data from CTD Seabird SBE 911Plus casts to
    calculate
  • Geostrophic currents along transects and Dynamic
    Height
  • Anomaly at levels
  • Plot ADCP current data perpendicular to cruise
    track
  • Obtain satellite and model products

3
Data Distribution
67
D
CUC
X
Y
Z
Q
R
77
4
Dynamic Height Anomaly at Surface
5
Sea Surface Height x Dynamic Height Anomaly
6
(No Transcript)
7
Dynamic Height Anomaly x ADCP
ADCP 15 to 25 m
8
(No Transcript)
9
Sea Surface Temperature
10
Temperature and Salinity Horizontal Sections at
250 m
11
Geostrophic Current
  • Assume CF HPGF, Hydrostatic Balance,
  • no acceleration, no friction and one level of no
    motion

adp dF -gdz
  • Geopotential distance between 2 isobaric surfaces
  • Geostrophic velocity at upper surface between
    stations
  • Matlab programs sw_gpan (geopotential anomaly)
  • and sw_gvel (geostrophic velocity) relative to
    the surface

12
ADCP x Geostrophic Currents
Line CUC
13
Sigma-t
14
Line Y
15
Sigma-t
16
Line X
17
Sigma-t
18
Line Q
19
Sigma-t
20
Factors that may lead to differences
  • Tide currents in shallow waters (depth to 200m)
  • Friction at Ekman Layers
  • Non-linearities due to eddies
  • Non-linearities due to Internal waves
  • Variation of wind stress

21
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