o3o3: A Variant of Spectral Elements with a Regular Collocation Grid

Author:

Steppeler J.1,Li J.2,Fang F.3,Zhu J.4,Ullrich P. A.5

Affiliation:

1. Climate Service Center, Hamburg, Germany

2. International Center for Climate and Environment Sciences, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China

3. Applied Modelling and Computation Group, Department of Earth Science and Engineering, Imperial College London, London, United Kingdom

4. International Center for Climate and Environment Sciences, Institute of Atmospheric Physics, Chinese Academy of Sciences, and Department of Atmospheric Sciences, University of Chinese Academy of Sciences, Beijing, China

5. Department of Land, Air and Water Resources, University of California, Davis, Davis, California

Abstract

AbstractIn this study, an alternative local Galerkin method (LGM), the o3o3 scheme, is proposed. o3o3 is a variant or generalization of the third-order spectral element method (SEM3). It uses third-order piecewise polynomials for the representation of a field and piecewise third-degree polynomials for fluxes. For the discretization, SEM3 uses the irregular Legendre–Gauss–Lobatto grid while o3o3 uses a regular collocation grid. o3o3 can be regarded as an inhomogeneous finite-difference scheme on a uniform grid, which means that the finite-difference equations are different for each group with three points. A particular version of o3o3 is set as an example of many possibilities to construct LGM schemes on piecewise polynomial spaces in which the basis functions used are continuous at corner points and function spaces having continuous derivatives are shortly discussed. We propose a standard o3o3 scheme and a spectral o3o3 scheme as alternatives to the standard method of using the quadrature approximation. These two particular schemes selected were chosen for ease of implementation rather than optimal performance. In one dimension, compared to standard SEM3, o3o3 has a larger CFL condition benefiting from the use of a regular collocation grid. While SEM3 uses the irregular Legendre–Gauss–Lobatto collocation grid, o3o3 uses a regular grid. This is considered an advantage for physical parameterizations. The shortest resolved wave is marginally smaller than that with SEM3. In two dimensions, o3o3 is implemented on a sparse grid where only a part of the points on the underlying regular grid are used for forecasting.

Funder

National Key Research and Development Program of China

China Postdoctoral Science Foundation Funded Project

Engineering and Physical Sciences Research Council

Publisher

American Meteorological Society

Subject

Atmospheric Science

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