Alpine Summer School 2010 - Course XVIII
"Buoyancy Driven Flows"
to be held in Valsavarenche, Valle d'Aosta (Italy), 21-30 June, 2010
Deadline for applications: April 26th, 2010:
http://to.isac.cnr.it/aosta/
Buoyancy is one of the main forces driving flows on our planet,
especially in the ocean and atmosphere. Buoyancy driven flows encompass
a wide spectrum of geophysical flows that range from buoyant coastal
currents to dense overflows in the ocean, and from avalanches to
volcanic pyroclastic flows on the Earth's surface.
The ocean displays an exceptionally wide range of buoyancy-driven
flows. Globally, buoyancy-driven currents are primarily responsible for
the redistribution of fresh water throughout the world's oceans and
play a key role in the global ocean circulation and climate change
through their impact on deep-water formation. Formation of dense water
usually occurs in marginal seas which are either cooler (at high
latitude) or saltier (due to a greater rate of evaporation). The dense
water enters the ocean as an entraining gravity-driven current (i.e. an
overflow), descending the continental slope (e.g. the Mediterranean
outflow into the North Atlantic) and entrains ocean water as it
descends. The final properties of dense current water masses are of
global importance since they become part of the global ocean
circulation. An understanding of the detailed flow behavior and the
entrainment/mixing by such dense currents is therefore critical to our
understanding of the stratification of the oceans. Finally, buoyant
coastal currents transport fresh water, heat, nutrients, sediments,
biogeochemicals, pollutants, and biological organisms along many
continental shelves and, hence, have important impacts on ecosystems,
fisheries, and the coastal circulation.
The lectures will first give a broad overview of the current
state-of-the-art research in buoyancy-driven flows and will be put in
the context of a wider range of geophysical problems (avalanches,
volcanic flows, atmospheric flows, etc.). Then, more specific lectures
will focus on the importance of correctly representing processes than
are not currently resolved in the ocean component of climate models.
Given the impact of buoyancy flows on the ocean circulation and the
earth's climate, we consider it timely to bring together leading
scientists to summarize our present theoretical, experimental, and
modeling understanding of buoyancy-driven flows.
One major objective of the school is to expose young graduate students
and recent Ph.D.s to the importance of buoyancy-driven flows in the
ocean circulation and in the present day climate from a combined
theoretical, experimental, and modeling point of view. The lecture
notes will be published as text book.
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