HR: 11:20h
AN: A32A-06 [Abstracts]
TI: Spatial scale separation of limited area models in the context of spectral nudging and isotropic
discrete filtering
AU: Feser, F
EM: feser@gkss.de
AF: Institute for Coastal Research,
GKSS Research Center, Max-Planck Strasse 1, Geesthacht, n/a 21502
Germany
AU: * von Storch, H
EM: storch@gkss.de
AF: Institute for Coastal Research,
GKSS Research Center, Max-Planck Strasse 1, Geesthacht, n/a 21502
Germany
AB:
The concept of spatial scale separation is analyzed in terms of model evaluation and dynamical downscaling techniques.
The main objective in downscaling is to obtain regional weather phenomena that are influenced by the local topography or
other small scale features. The continental scale atmospheric state is assumed to be well resolved in global reanalyses data
and thus it is to be retained by a regional model.
For some meteorological conditions, like blocking weather situations, a regional model may simulate large scale features
which do no agree with the large scale state of the global forcing data. The application of a spectral nudging technique
forces the regional model to approximate the large
scales to the reanalysis data for the whole integration area while the small scales are computed exclusively by the regional
model.
Large-scale control of regional climate modeling overcomes the fundamental problem of dealing with an ill-posed boundary
value problem, but its usefulness depends on the specific application. The method of spectral nudging in regional climate
modeling is discussed, and its utility in forcing the known large-scale state without suppressing regional and local
variability is demonstrated.
Also, spatial scale separation can be used for limited area model evaluation purposes. A two-dimensional discrete filter was
developed which serves as a tool to classify meteorological fields according to their spatial dimensions by filtering certain
wave number ranges. Thereby it performs an isotropic spatial scale separation of the limited area model fields.
The filter algorithm is presented and examples demonstrate the scale separation of atmospheric fields on limited area grids
which can be used for model evaluation, comparisons or process studies.
DE: 3337 Numerical modeling and data assimilation
DE: 3319 General circulation
DE: 1620 Climate dynamics (3309)
SC: Atmospheric Sciences [A]
MN: 2004 AGU Fall Meeting