Articles | Volume 9, issue 5
Geosci. Model Dev., 9, 2007–2029, 2016
https://doi.org/10.5194/gmd-9-2007-2016
Geosci. Model Dev., 9, 2007–2029, 2016
https://doi.org/10.5194/gmd-9-2007-2016

Development and technical paper 01 Jun 2016

Development and technical paper | 01 Jun 2016

A high-order staggered finite-element vertical discretization for non-hydrostatic atmospheric models

Jorge E. Guerra and Paul A. Ullrich Jorge E. Guerra and Paul A. Ullrich
  • Department of Land, Air and Water Resources, University of California, Davis, One Shields Ave., Davis, CA 95616, USA

Abstract. Atmospheric modeling systems require economical methods to solve the non-hydrostatic Euler equations. Two major differences between hydrostatic models and a full non-hydrostatic description lies in the vertical velocity tendency and numerical stiffness associated with sound waves. In this work we introduce a new arbitrary-order vertical discretization entitled the staggered nodal finite-element method (SNFEM). Our method uses a generalized discrete derivative that consistently combines the discontinuous Galerkin and spectral element methods on a staggered grid. Our combined method leverages the accurate wave propagation and conservation properties of spectral elements with staggered methods that eliminate stationary (2Δx) modes. Furthermore, high-order accuracy also eliminates the need for a reference state to maintain hydrostatic balance. In this work we demonstrate the use of high vertical order as a means of improving simulation quality at relatively coarse resolution. We choose a test case suite that spans the range of atmospheric flows from predominantly hydrostatic to nonlinear in the large-eddy regime. Our results show that there is a distinct benefit in using the high-order vertical coordinate at low resolutions with the same robust properties as the low-order alternative.

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Short summary
This work introduces a collection of advances in the field of numerical simulation of the atmosphere using mixed finite element methods. We emphasize vertical motions in the atmosphere and apply state-of-the-art mathematics and programming paradigms to solve the differential equations that govern air flow cast in a coordinate-free formulation. The simulations show accurate flow features over a wide range of spatial scales including several important phenomena.