| In nearly all applications,
the answer is no. More than 25 years ago, it was observed
that OBS sensors deployed under breaking waves were virtually
unaffected by entrained bubble clouds. This was puzzling because
bubbles scatter light by the same general mechanism as any suspended
particle having an index of refraction different than water.
Surf and whitecaps produce extreme bubble concentrations but
mountain streams flowing over boulders and propellers wakes
also produce a lot of aeration. The key factors that determine
whether or not bubbles will interfere with OBS measurements
are their backscatter efficiency, size, and concentration.
Bubbles and foam appear all over the place. So why
are they not a big problem? Back-scattering efficiency
is the dimensionless ratio of the scattering area to the cross-sectional
area of the particle. A high-efficiency scatterer reflects
more light back toward an emitter than a low efficiency one.
This is analogous to taking the product of absorptivity and
concentration to estimate the absorption of dissolved, material
(see absorption effects).
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The VSF for bubbles, in the
range of scattering angles from 100° to 170° lies
between those for organic material and minerals. Most significantly,
the VSF values are about 80% less than for minerals and this
means it takes about five times more bubbles than mineral
particles to produce the same intensity of light scattering,
other things being equal. Bubble size and concentration are
more important than efficiency because these factors can vary
by more than a factor of 100 in the environment. In order
to determine if bubbles interference is significant, we reviewed
bubble concentration data taken under breaking waves and compared
the maximum observed bubble concentrations in the silt-sand-size
range with the threshold concentration of sand (10 mg l-1)
needed to produce measurable OBS signals. The maximum bubble
concentration is about an order of magnitude less than threshold
SSC for sand. So, when low backscatter efficiency is combined
with low bubble concentration, we find that bubbles are not
of concern even in foamy, aerated environments, and the visual
effects of bubbles and foam are misleading. |
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Reference:
John Downing and W.E. Asher. The Effects of Colored
Water and Bubbles on the Sensitivity of OBS Sensors.
American Geophysical Union, 1997 Fall Meeting, San Francisco,
CA.
Terrill, E.J., W.K. Melville, & D. Stramski. 1998. Bubble
Entrainment by Breaking Waves and Their Effects on the Inherent
Optical Properties of the Upper Ocean. Proceedings
of Ocean Optics XIV.
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