Hj. Herzog, TESTING A RADIATIVE UPPER BOUNDARY-CONDITION IN A NONLINEAR MODEL WITH HYBRID VERTICAL COORDINATE, Meteorology and atmospheric physics, 55(3-4), 1995, pp. 185-204
The application of a radiative upper boundary condition (RUBC) in a me
soscale numerical weather prediction (NWP) model with hybrid vertical
coordinate is presented. Results of two- and three-dimensional numeric
al simulations are discussed. Starting from earlier work by Klemp and
Durran (1983) and Bougeault (1983) the radiative upper boundary condit
ion is formally derived for a hybrid vertical coordinate. The basic as
sumptions include hydrostaticity, linearity, neglect of Coriolis effec
ts and restriction to internal gravity waves. The resulting RUBC is gl
obal in space and local in time. In a second step, the RUBC is tested
in a two-dimensional vertical-plane version of the NWP model, in which
essential properties of the full three-dimensional model have been pr
eserved. Gravity wave experiments clearly show the superiority of the
RUBC over the commonly used lid-type upper boundary condition. For the
setting with an isolated bell-shaped mountain with resolution-indepen
dent steepness, the RUBC tends to work more effectively with increasin
g horizontal resolution. At the same time, the application of a radiat
ive instead of a lid-type, and thus reflecting, upper boundary conditi
on appears to become more important with decreasing mesh width. Finall
y, the RUBC is introduced into the full three-dimensional NWP model. T
his requires further approximations. In particular for a limited-area
model, the geopotential field at the uppermost model level needs to be
bi-periodic. Here, a linear detrending technique is applied. First re
sults for a weather situation with strong northwesterly flow towards t
he Alps show that application of the RUBC drastically reduces the deve
lopment of unrealistic standing, hydrostatic mountain waves, which bec
ome apparent as distinct mesoscale ridge-trough structures in the simu
lation with the lid-type upper boundary. Implications of the RUBC on t
he time-stepping procedure of the NWP model are also discussed. In the
experiments shown, the additional RUBC-terms are treated explicitly.