Consistent approximate models of the global atmosphere: shallow, deep, hydrostatic, quasi‐hydrostatic and non‐hydrostatic
By A. White, B. Hoskins, I. Roulstone, Andrew Staniforth. 2005
156 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/2f43de792a9d081157b201cd1b26fed50fa5def1
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Global and Planetary Change
- David L. Williamson
- Christiane Jablonowski
- R. Akmaev
- C. Charlton-Perez
- John Thuburn
- Chris Smith
- Susan P. Ballard
- Peter A. Clark
In Oceanography
- R. Akmaev
- Christiane Jablonowski
- David L. Williamson
- John Thuburn
- Leo R. M. Maas
- S. Vosper
- Andrew Staniforth
- W. Melville
Citations in the corpus
- Geophysical and astrophysical fluid dynamics beyond the traditional approximation (2008, background): “This has led several authors [White and Bromley, 1995; Marshall et al., 1997; White et al., 2005] to propose an alternative, the quasihydrostatic approximation, which means that one replaces (10) by an equation from which only the material derivative is removed: ~f u ¼ 1 r @p @z g; ð13Þ the…”
- An inherently mass‐conserving semi‐implicit semi‐Lagrangian discretization of the deep‐atmosphere global non‐hydrostatic equations (2014, background): “(21), such that the deepatmosphere equation set is fully non-hydrostatic when δV ≡ 1 but reduces to the quasi-hydrostatic equation set (White et al., 2005) when δV ≡ 0.”
- Convection‐permitting models: a step‐change in rainfall forecasting (2016, background): “As a result, until recently, the majority of NWP models were based on the hydrostatic primitive equations (HPEs) (White et al., 2005).”
- The pros and cons of diffusion, filters and fixers in Atmospheric General Circulation Models (2011, methodology): “The replacement of the distance r by a is in fact a necessity in hydrostatic models based on the primitive equations (White et al. 2005).”
- WHOLE ATMOSPHERE MODELING: CONNECTING TERRESTRIAL AND SPACE WEATHER (2011, methodology): “The three approximations have often been applied together to the Navier‐Stokes equations to derive the so‐called “primitive equations,” a long‐standing framework for atmospheric and oceanic GCMs, but they do not have to be adopted simultaneously [e.g., Veronis, 1968; Phillips, 1968; White et al., 20”