Sea-Bird Electronics SBE 38 Manual de usuario Pagina 75

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Manual revision 006 Section 4: Deploying and Operating SBE 19plus V2 SBE 19plus V2
75
When very heavy seas cause severe ship motion, the 19plus V2 descent can
actually stop or reverse direction if the ship heaves upward faster than the
package can descend. These occurrences can often be seen as loops in the real-
time temperature trace. If the winch payout rate is too high, a loop of wire can
form under water when the package descent is slowed or reversed by ship
heave and the winch is still paying out wire. Inevitably, the loop formation
gets out of phase with the heave and the loop closes on itself when the ship
heaves, causing a kink. If the package includes a Carousel Water Sampler as
well as the CTD, the package creates much more drag than with only the CTD,
further increasing the possibility that a loop will form in the cable. After
1000 to 2000 meters of cable are paid out, it can be difficult or impossible to
detect a loop in the cable. Adding 100 to 200 kg (maybe more by
experimentation) of lead weights to the Carousel frame will help overcome the
effect of drag, and allow the package to descend faster and stay more in line
directly below the overboarding sheave.
Spiking is sometimes seen in the derived values for salinity, density, or sound
velocity. Spiking results largely from a response time mismatch of the
conductivity and temperature sensors, especially when the profiling descent
rate is non-uniform. The greatest reduction in spiking is found by using
premium CTD equipment such as the SBE 9plus, which uses very fast sensors
(0.07 second) and high speed (24 Hz) parallel signal acquisition. The 19plus
V2 static accuracy is the same as that of the 9plus, but its dynamic responses
are not as ideal, as a result of its simpler, less costly, and more compact
design. Much of the spiking can be removed from the data set by aligning the
data in time. This alignment can be performed when post-processing the data
in SBE Data Processing.
The amount of spiking depends on the temperature gradient, and is much
worse when coupled surface motion causes the instrument to stop - or even
reverse - its descent. In the event of heavy ship motion, it may be worth letting
the instrument free-fall. When very heavy seas cause severe ship motion and
result in periodic reversals of the instrument descent, the data set can be
greatly improved by removing scans taken when the pressure is not increasing,
using SBE Data Processing.
Note:
See the SBE Data Processing
manual for information on data
processing modules that can correct
data for the influences of ship motion
and minimize salinity spiking.
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