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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Main Authors: S. Borchert, G. Zhou, M. Baldauf, H. Schmidt, G. Zängl, D. Reinert
Format: Article
Language:English
Published: Copernicus Publications 2019-08-01
Series:Geoscientific Model Development
Online Access:https://www.geosci-model-dev.net/12/3541/2019/gmd-12-3541-2019.pdf
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spelling 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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