The upper-atmosphere extension of the ICON general circulation model (version: ua-icon-1.0)
<p>How the upper-atmosphere branch of the circulation contributes to and interacts with the circulation of the middle and lower atmosphere is a research area with many open questions. Inertia–gravity waves, for instance, have moved in the focus of research as they are suspected to be key featu...
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doaj-19b90139b171475f982dc9af9156e61a2020-11-24T20:51:23ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032019-08-01123541356910.5194/gmd-12-3541-2019The upper-atmosphere extension of the ICON general circulation model (version: ua-icon-1.0)S. Borchert0G. Zhou1G. Zhou2M. Baldauf3H. Schmidt4G. Zängl5D. Reinert6Deutscher Wetterdienst, Offenbach am Main, GermanyMax Planck Institute for Meteorology, Hamburg, Germanycurrently at: College of Oceanography, Hohai University, Nanjing, ChinaDeutscher Wetterdienst, Offenbach am Main, GermanyMax Planck Institute for Meteorology, Hamburg, GermanyDeutscher Wetterdienst, Offenbach am Main, GermanyDeutscher Wetterdienst, Offenbach am Main, Germany<p>How the upper-atmosphere branch of the circulation contributes to and interacts with the circulation of the middle and lower atmosphere is a research area with many open questions. Inertia–gravity waves, for instance, have moved in the focus of research as they are suspected to be key features in driving and shaping the circulation. Numerical atmospheric models are an important pillar for this research. We use the ICOsahedral Non-hydrostatic (ICON) general circulation model, which is a joint development of the Max Planck Institute for Meteorology (MPI-M) and the German Weather Service (DWD), and provides, e.g., local mass conservation, a flexible grid nesting option, and a non-hydrostatic dynamical core formulated on an icosahedral–triangular grid. We extended ICON to the upper atmosphere and present here the two main components of this new configuration named UA-ICON: an extension of the dynamical core from shallow- to deep-atmosphere dynamics and the implementation of an upper-atmosphere physics package. A series of idealized test cases and climatological simulations is performed in order to evaluate the upper-atmosphere extension of ICON.</p>https://www.geosci-model-dev.net/12/3541/2019/gmd-12-3541-2019.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
S. Borchert G. Zhou G. Zhou M. Baldauf H. Schmidt G. Zängl D. Reinert |
spellingShingle |
S. Borchert G. Zhou G. Zhou M. Baldauf H. Schmidt G. Zängl D. Reinert The upper-atmosphere extension of the ICON general circulation model (version: ua-icon-1.0) Geoscientific Model Development |
author_facet |
S. Borchert G. Zhou G. Zhou M. Baldauf H. Schmidt G. Zängl D. Reinert |
author_sort |
S. Borchert |
title |
The upper-atmosphere extension of the ICON general circulation model (version: ua-icon-1.0) |
title_short |
The upper-atmosphere extension of the ICON general circulation model (version: ua-icon-1.0) |
title_full |
The upper-atmosphere extension of the ICON general circulation model (version: ua-icon-1.0) |
title_fullStr |
The upper-atmosphere extension of the ICON general circulation model (version: ua-icon-1.0) |
title_full_unstemmed |
The upper-atmosphere extension of the ICON general circulation model (version: ua-icon-1.0) |
title_sort |
upper-atmosphere extension of the icon general circulation model (version: ua-icon-1.0) |
publisher |
Copernicus Publications |
series |
Geoscientific Model Development |
issn |
1991-959X 1991-9603 |
publishDate |
2019-08-01 |
description |
<p>How the upper-atmosphere branch of the circulation contributes to
and interacts with the circulation of the middle and lower atmosphere
is a research area with many open questions. Inertia–gravity waves, for instance,
have moved in the focus of research as they are suspected to be key features
in driving and shaping the circulation. Numerical atmospheric models are
an important pillar for this research. We use the ICOsahedral Non-hydrostatic
(ICON) general circulation model, which is a joint development
of the Max Planck Institute for Meteorology (MPI-M)
and the German Weather Service (DWD), and provides, e.g., local mass conservation,
a flexible grid nesting option, and a non-hydrostatic dynamical core
formulated on an icosahedral–triangular grid.
We extended ICON to the upper atmosphere and present here the two main components
of this new configuration named UA-ICON: an extension of the dynamical core from
shallow- to deep-atmosphere dynamics and the implementation of an upper-atmosphere
physics package.
A series of idealized test cases and climatological simulations is performed
in order to evaluate the upper-atmosphere extension of ICON.</p> |
url |
https://www.geosci-model-dev.net/12/3541/2019/gmd-12-3541-2019.pdf |
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