[GTP] MMM SEMINAR 7/28/10 @ 10:30AM--Mironov
Silvia Gentile
sgentile at ucar.edu
Wed Jul 21 10:33:15 MDT 2010
MMM SEMINAR NCAR
Effect of Surface Temperature Heterogeneity on Turbulent Mixing in a
Stably Stratified Atmospheric Boundary Layer
Dmitrii V. Mironov
German Weather Service, Offenbach am Main, Germany
Peter P. Sullivan National Center for Atmospheric Research, Boulder CO, USA
Idealized LES of two stably stratified boundary layer (SBL) flows driven
by fixed winds and homogeneous and heterogeneous surface temperature are
compared. The LES data are used to compute statistical moments of the
fluctuating fields (mean wind and mean potential temperature,
second-order and third-order turbulence moments, pressure-velocity and
pressure-scalar co-variances), to estimate terms in the second-moment
budgets, and to assess the relative importance of various terms in
maintaining the budgets. The budgets of the turbulence kinetic energy
(TKE), of the temperature variance, and of the vertical temperature flux
are analyzed. As different from most previous studies, the LES-based
second-moment budgets are estimated with due regard for the sub-grid
scale contributions. These contributions may be substantial,
particularly in the SBL, and should be retained in order to close the
second-moment budgets to a good order. We find the SBL over a
heterogeneous surface is more turbulent with larger variances and TKE,
is better mixed and is deeper compared to its homogeneous counterpart.
The latter results are similar to those described by Stoll and
Porte-Agel (2009). Perhaps the most striking difference between the
cases is exhibited in the temperature variance and its budget. Due to
surface heterogeneity, the third-order moment, i.e. the vertical flux of
temperature variance, is non-zero at the surface. Hence, the turbulent
transport term (divergence of the above third-order moment) not only
redistributes the temperature variance in the vertical, but is a net
gain. As a result, the temperature variance in the heterogeneous case is
large near the surface. Motivated by the LES results, possible ways to
incorporate the effect of the sub-grid scale surface temperature
heterogeneity into the SBL turbulence models (parameterization schemes),
including the surface-layer flux-profile relationships, are discussed.
Wednesday, 28 July 2010, 10:30 AM
Refreshments 10:15 AM
NCAR-Foothills Laboratory
3450 Mitchell Lane
Bldg 3, Room 2072
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