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Small Scales and Extreme Events: The HurricaneFebruary 12 - 16, 2007Schedule and PresentationsProgram Poster PDFHotel Accommodations and Air TravelOrganizing Committee
Kayo Ide
(University of California, Los Angeles (UCLA), Atmospheric Sciences)
Scientific BackgroundTwo central issues in the predictability of geophysical flows are how to predict extreme events, and how to represent the collective effects of small-scale energetic processes. These grand themes are well illustrated by the tropical cyclone, a large-scale convective storm system in the tropical atmosphere that rotates counterclockwise in the northern hemisphere and draws its fuel principally from the evaporation of ocean water when the low-level winds attain sufficient strength. Intense tropical cyclones over the Atlantic are called hurricanes; similar storms in the North Pacific are called typhoons. Hurricanes and typhoons are among the fiercest storms conjured by nature, whose destructive power has become apparent to all over the last several years.
From the perspective of climate science the frequency and average intensity
of tropical cyclones is also a question of great
importance. The former requires an understanding of the mechanisms of
cyclogenesis, a long standing and enigmatic problem in both tropical
meteorology and geophysical fluid dynamics; the latter demands an
understanding of how various physical processes interact to regulate
intensity variations in storms. Both are questions at the forefront of
contemporary research on the fluid dynamics and thermodynamics of tropical
storms. Both are also challenging problems in moist vortex dynamics, the dry
counterpart of which has a distinguished tradition within applied
mathematics. A central issue in the cyclogenesis problem, for example,
involves understanding how horizontally small-scale (order 10 km) hot towers
(cumulonimbus clouds) create a self-sustaining large-scale vortex. The hot
towers, and the coherent vortex wave structures they are embedded in, are
believed to mediate the transfer of energy from the underlying ocean. These
coherent structures are also believed to regulate intensification cycles in
intense hurricanes/typhoons. The small-scale/large-scale interaction Modern simulation methods being used to study hurricanes include fine-scale modeling of incipient storms, and hierarchical modeling of the entire system. Short-term predictions of tropical cyclone genesis and evolution requires accurate model initialization. This involves properly capturing both the nature of the underlying balanced flow, and the small scale features (cumulonimbus ``hot'' towers) it organizes---in ways which can be amplifying or not. The initialization problem proves to be a great challenge for modern data assimilation. Another theme of the workshop will thus be to explore techniques related to stochastic data assimilation, and information theory. On longer-time and larger-space scales, new techniques are being developed that involve normal (non-hierarchical) multi-scale methods. While bearing some resemblance to recent work in applied mathematics on hierarchical multi-scale methods, there are important differences (principally related to scale separation assumptions). The third element of the workshop will thus be to explore how to interpret the representation of tropical cyclones by such techniques, and the extent to which they provide a meaningful basis for predicting the intensity and frequency of hurricanes in other climates.
GOALS: SpeakersJoseph Biello (University of California, Davis (UC Davis))Kristen Corbosiero (National Center for Atmospheric Research) Kerry Emanuel (Massachusetts Institute of Technology) Bjorn Engquist (University of Texas at Austin) Wojciech Grabowski (National Center for Atmospheric Research) John Harlim (New York University) Isaac Held (Geophysical Fluid Dynamics Laboratory/NOAA) Keith Julien (University of Colorado, Boulder) Markos Katsoulakis (University of Massachusetts Amherst) Richard Kleeman (New York University) Rupert Klein (Freie Universität Berlin) Andrew Majda (New York University) Michael Montgomery (Naval Postgraduate School) David Randall (Colorado State University) Wayne Schubert (Colorado State University) Roger Smith (Ludwig-Maximilians-Universität München) Chris Snyder (National Center for Atmospheric Research) Joseph Tribbia (National Center for Atmospheric Research) Xiaoming Wang (Florida State University) Xiaolei Zhou (Florida State University) Contact Us:Institute for Pure and Applied Mathematics (IPAM) |
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