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Geophysical Turbulence Program Workshop
Turbulence and Scalar Transport in Roughness Sublayers
26-28 September 2006; Boulder, Colorado, USA
Venue:
The National Center for Atmospheric Research
3450 Mitchell Lane
Boulder, Colorado, USA
Foothills Laboratory, Building 2
Main Seminar Room
Organizing Committee:Don Lenschow (MMM/NCAR), Steven
Oncley (EOL/NCAR), Ned Patton (MMM/NCAR), Peter Sullivan
(MMM/NCAR), Jielun Sun (MMM/NCAR), Jeffrey Weil (University of
Colorado), Peggy LeMone (MMM/NCAR), Chin-Hoh Moeng (MMM/NCAR),
Tom Horst (EOL/NCAR)
The National Center for Atmospheric Research will host a
workshop in Boulder, Colorado, September 26-28, 2006 sponsored
by the Geophysical Turbulence Program (GTP). The workshop will
bring together researchers interested in the roughness
sublayer; the layer of flow immediately above (or below) a
boundary surface (air-land or air-water interface) containing
stationary and moving roughness elements, such as stones,
vegetation (trees), buildings, wind turbines, or water
waves. The approaches considered are numerical and laboratory
modeling, observations, and theory.
Scientific Background and Rationale:
The roughness sublayer normally extends from the interface up
to about two to several times the height of the roughness
elements. Within the roughness sublayer the flow is
three-dimensional and site-dependent since it is dynamically
influenced by the length scales and density/porosity of the
individual roughness elements. Turbulence properties and scalar
transport (including deposition) may vary with the surface type
and texture, e.g., bluff obstacles in cities versus the fibrous
"fine-grained" elements of vegetation.
In general, Monin-Obukhov (M-O) similarity theory successfully
predicts mean and turbulence statistics in the surface layer above the
roughness sublayer, but is not applicable within the roughness
sublayer as turbulence and local circulations are strongly affected by
individual roughness elements. The transport of passive scalars
(e.g., CO2, water vapor, other trace gas species, and aerosols) can be
quite different from dynamical quantities such as temperature and
momentum. For example, pressure drag dominates momentum transport
within the roughness elements while passive species are not so
constrained. Turbulent eddies in roughness sublayers are particularly
anisotropic and highly intermittent in space and time, especially
under stable situations. The complicated nature of turbulence within
the roughness sublayer also dramatically influences chemical reaction
rates.
Roughness sublayers develop in geophysical flows over a myriad of
surfaces, including those containing forests, hills, wind farms,
cities, and even bare soil. Oceanic waves present a special problem in
that the underlying "roughness" (the wave field) propagates at
directions not necessarily related to the local wind and because of
wave breaking which leads to multiphase flows near the air-water
interface. There is an increasing need to understand turbulence in
these complicated regimes; e.g., monitoring the global carbon budget,
parameterizing boundary-layer flow, deploying observational networks,
simulating urban pollutant dispersion, forecasting hurricanes, and
predicting extreme events. Since there are currently no viable
parameterization schemes to adequately describe the structure of flow
in roughness sublayers, numerical models typically rely on M-O
similarity to bridge the gap between the outer regions of the flow and
surfaces, despite the known shortcomings. Indeed, the roughness
sublayer is likely one of the weakest links among the entire suite of
boundary layer parameterizations in global and mesoscale models.
Workshop Format:
The workshop will feature a series of invited talks,
interspersed with discussion sessions, and short contributed
oral presentations. The invited talks will focus on recent
observational, numerical modeling, and laboratory simulation
results to better understand turbulence structure and transport
in roughness sublayers. The discussions will focus on
fundamental issues related to the roughness sublayer and how we
deal with the roughness sublayer in a variety of
applications. A summary paper is planned to be submitted to a
scientific publication.
Voluntary abstract submission:
Anyone who wishes to give a brief oral presentation is required
to provide a one-page (maximum) abstract by 1 June 2006.
Submission of an abstract does not guarantee that you will be speaking,
since there may not be enough time to include all who wish to speak.
Please email your abstract (in pdf format) to
Liz Rothney rothney "at" ucar .dot. edu
Extended abstract for invited speakers:
All invited speakers should email a 2-page extended
abstract (in pdf) to Liz Rothney
rothney "at" ucar .dot. edu by
15 August 2006.
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