Abstract
Abstract. This article describes the implementation of grid refinement in the ICOsahedral Nonhydrostatic (ICON) modeling system.
It basically follows the classical two-way nesting approach known from widely used mesoscale models like MM5
or WRF, but it differs in the way feedback from fine grids to coarser grids is applied.
Moreover, the ICON implementation supports vertical nesting in the sense that the upper boundary of a nested domain
may be lower than that of its parent domain. Compared to the well-established implementations on quadrilateral grids,
new methods had to be developed for interpolating the lateral boundary conditions from the parent domain to the
child domain(s). These are based on radial basis functions (RBFs) and partly apply direct reconstruction of the
prognostic variables at the required grid points, whereas gradient-based extrapolation from parent to child grid
points is used in other cases.
The runtime flow control is written such that limited-area domains can be processed identically to nested domains
except for the lateral boundary data supply. To demonstrate the functionality and quality of the grid nesting in ICON,
idealized tests based on the Jablonowski–Williamson test case (Jablonowski and Williamson, 2006) and the Schär mountain wave
test case (Schär et al., 2002) are presented. The results show that the numerical disturbances induced at the nest
boundaries are small enough to be negligible for real applications. This is confirmed by experiments closely
following the configuration used for operational numerical weather prediction at DWD, which demonstrate that a
regional refinement over Europe has a significant positive impact on the forecast quality in the Northern
Hemisphere.
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