Seismic Oceanography
In early 2003, I was privileged to review the first, seminal paper on
SO (Holbrook et al. 2003). This paper showed that
sound reflects strongly enough from thermal structures in the water
column that the reflected sound could be used to determine the size,
location, and temperature contrast of the features. This meant that
multichannel seismic observations can image fine-structure within the
oceanic water column with unprecedented (~10m) resolution. On the
basis of my enthusiastically positive review I was asked to write a
Science Perspectives article (Ruddick, 2003) on the prospects
for this new tool. I noted that the seismic images are analogous to
satellite images, giving lots of detail, but working best when
combined with quantitative physical oceanographic observations. I was
also interviewed by Deutschland Radio on the same topic ("Forschung
Aktuall", 12-08-2003).
Ruddick et al. 2009, showed how seismic reflection images vertical
temperature gradient averaged on scales of 5-10 m, exactly the
quantity oceanographers would like detailed maps of in order to show
the fine structures related to mixing phenomena like intrusions and
internal waves.
(Left) Contours of thickness of a penny. (Right) Grayscale image of
vertical gradient of thickness. The image at left is the way
oceanographers traditionally plot observations; the image at right,
much richer in detail and looking like a penny illuminated from above,
is analogous to a seismic image. The figures below illustrate the
same point for CTD-derived and seismic images of a real oceanic Meddy,
an eddy containing water from the Mediterranean often found in the
Atlantic.
I took part as a foreign participant in the large EU project
"Geophysical Oceanography", leading to many collaborations, past and
present, with the Prof. Luis Pinheiro.s group at the University of
Aveiro, Portugal. We are imaging Meddies, fronts, currents, and other
structures using the technique, and doing our best to learn new
quantitative things about ocean mixing.
(Left) Conventional contour plot of temperature from a CTD transect of
Meddy Sharon (Armi et al., 1989). The CTD casts have a vertical
resolution of a few meters, but are spaced more than 1.5 km
apart. Contour interval is 2°, with red indicating 18-20°. (Right)
Seismic oceanography image from the IAM5 section on the Iberian margin
during the Iberian Atlantic Margins Project showing a previously
undiscovered meddy, with strong fine-structure reflectors surrounding
the meddy core, and relatively few reflectors in the core. Seismic
images such as this one show structures like meddies because sound
reflects from the fine-scale temperature and salinity variations that
are most intense near their edges. The vertical axis at left is
two-way travel time (TWT).the time required for sound to travel
vertically from the surface to the reflector and back to the
surface. The axis at right is the equivalent depth based on a sound
velocity of 1500 m s-1. Upper axis is the common midpoint (CMP) value,
with 1CMP = 12.5 m. Lower x-axis is west longitude along the nearly
east-west section. (Pinheiro et al, 2009)
Collaborations in this new field continue to expand. I was invited to
attend and give two keynote lectures at an EU-funded Workshop on
Seismic Oceanography in Begur, Spain, November 2008, a small
Gordon-Conference-like meeting with about 80 participants. I was
recently invited to take part as a foreign participant in a new EU
project (POSEIDON) on Seismic Oceanography based in Barcelona, Spain.
Dr. Berta Biescas, of the Unitat de Tecnologia Marina in Barcelona,
Spain, was recently awarded a Curie Fellowship to come to Dalhousie in
2011-2013 to work with me and Mladen Nedimovic. The focus of the
project is quantitative inversion of seismic data to obtain
temperature and salinity using seismic observations. to remotely infer
thermohaline structure in the water column.
A group of us at Dalhousie and BIO successfully intercompared seismic
and hydrographic observations South of Nova Scotia. The objective was
to "ground truth" a Multichannel Seismic survey with detailed
oceanographic observations. Mirshak et al (2010) give a detailed
comparison of seismic images from the Gulf Stream frontal region with
hydrographically-derived synthetic images showing fronts, eddies,
tendrils and interleaving in both data sets, one of the best
intercomparisons between seismic and hydrographic profiling to date.
The resulting data set is one of only a few suitable for development
and testing of techniques for "quantitative inversion" - the inversion
of seismic data to obtain detailed oceanographic information such as
temperature gradient, temperature, and salinity, a project we hope to
begin soon with Mladen Nedimovic and Berta Biescas.