Title: A%20Comparison%20of%20Six%20Expendable%20Bathythermograph%20Data%20Acquisition%20Systems
1A Comparison of Six Expendable Bathythermograph
Data Acquisition Systems
Derrick Snowden Molly Baringer Gustavo Goni
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3Instruments List
366 total profiles
4XBT Errors
A
B
- XBT differs from the CTD due to
- A inaccurate depth measurements
- B inaccurate temperature measurements
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8Fall Rate Error Initial Conditions
Hallock and Teague 1992
9Fall Rate Equation
e.g. Hallock and Teague (1992)
a Change of mass of the probe due to spooling
wire. b Probe geometry and initial terminal
velocity c Describes startup transients i.e.
initial conditions
Currently used FRE (WMO 177052) for Deep Blue
probes contains no constant term ( c ).
10Determining Depth Offset
Hanawa et al (1995)
Focus on the temperature gradient derivative of
temperature with respect to depth Minimize
temperature error effect
11Depth Offset Prior to Correction
12Depth Correction Algorithm
- Assemble the depth offsets (dZ)
- Recalculate XBT depths
- Znew ZxbtdZ
- Back calculate time (t)
- Fit new fall rate equation to (t)
- z at2 bt c
13Depth Offset Post-Correction
14Summary of Fall Rate Coefficients
A B C
Wmocode 52 -0.00225 6.691 0
this study -0.00191 6.487 0
this study -0.00299 6.639 -4.5117
other studies (1) -0.00131 -0.00329 6.440 6.798 0 - 0
1 Taken from Hanawa et al 1995
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