"I've
got a whale of a tale to tell you lads, a whale of a tale or two..."
During
the first two weeks of August 200, Dr. Richard Styles and lab tech
Dara Hooker participated in a research cruise off the coast of Charleston,
SC aboard the research vessel Seward Johnson . This project
was funded by the National Oceanic and Atmospheric Administration
(NOAA) Ocean Explorer Program. Click
here to go to their comprehensive website which chronicles the
entire cruise. We were part of a research group studying the physical
and biological dynamics of the Charleston Bump, a geological feature
which rises approximately 300 meters from the sea floor off the
coasts of South Carolina and Georgia and impacts the flow of the
Gulf Stream. In addition to Dr. Styles and Dara, other participating
USC members included Steve Stancyk, Brian Helmuth, Denise Stickland,
and Frank Helies. The scope of the cruise was largely exploratory,
but our specific goal was to characterize how the local hydrodynamic
conditions affect the benthic invertebrate communities in the area.
An amazing amount of data was collected, including biological and
geological samples from the seafloor, hours and hours of video from
the sub dives, and 2 weeks worth of ADCP current data and CTD cast
data. The data from the ADCPs and CTD casts will form the basis
of Dara's thesis work. The trip was an experience that we will never
forget. We traveled 1800 feet to the bottom of the Atlantic Ocean
and came back to tell the tale!
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Dr.
Styles (left) and Dara Hooker (second from left) represented
the BLASST Lab. Also pictured (left to right): Jerry, Phil,
and Betty |
CTD
(Conductivity, Temperature, and Depth) sensors attached to
a metal rosette frame. |
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Dara,
prepared for inclement weather! |
How
many scientists does it take to operate a pipe dredge? This
custom pipe dredge will collect samples from the bottom for
analysis. |
 |
| Critters
from the Charleston Bump, brought to light by the intrepid
sub crew:
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bathynectes |
.carrion
shrimp |
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really
cool rock |
sponge |
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toadfish
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| These
are clod cards, shown before deployment on the left and
after deployment on the right. These are plaster of Paris
cards that dissolve at a fixed rate. By measuring the
rate of erosion, one can estimate the shear stress near
the sea bed. Thus, clod cards are a relatively inexpensive
method for measuring near bottom flow patterns. |
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Oceanography...not
for the faint of heart...or weak of stomach!
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