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Physical/Chemical
Oceanography: Dr. Trevor J.
McDougall, of the Commonwealth
Scientific and Industrial Research
Organization (CSIRO) in Australia, for
his leading role in developing a
practical understanding of important
thermodynamic and dynamic processes in
the ocean, which are a key to the
determination of the mixing motions that
so strongly influence ocean circulation
and heat transport.
Dr. McDougall is a Chief Research
Scientist in the Division of Marine
Research and Leader of the Climate
Research Group at CSIRO in Hobart,
Australia. He holds an Honours Degree in
Mechanical Engineering from the
University of Adelaide, a Ph.D. in
Applied Mathematics and Theoretical
Physics from Cambridge University, and a
Graduate Diploma in Economics from the
Australian National University. He is a
Fellow of the Australian Academy of
Science, and recipient of the Frederick
White Prize awarded by the Australian
Academy of Science, and the Banks Medal
from the Royal Society of Tasmania.
Dr. McDougall has used a combination
of physical insight and mathematical
formalism to elucidate fundamental
effects associated with nonlinearities in
the relationship between sea water
density and temperature, salinity and
pressure, and to bring order and rigour
to the study of a range of complex ocean
processes that had defied previous
efforts. His work has covered ocean
processes on spatial scales ranging from
centimeters to hundreds of kilometers. At
the smallest scales, Dr. McDougall has
used laboratory experiments, theory and
ocean observations to understand and
reveal the links between turbulence,
"double diffusion",
"cabbeling", entrainment and
subtle thermodynamic effects. On larger
scales, he has defined the "neutral
density surfaces" along which
energetic mesoscale eddies mix in the
ocean, and he has developed dynamically
consistent parameterizations to represent
mesoscale mixing processes in ocean
models. Many aspects of his work have
become basic building blocks in
state-of-the-art ocean general
circulation models. His truly original
contributions are having major influences
on ocean studies ranging from the
smallest-scale mixing processes to the
understanding of global ocean climate and
its implications
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