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  ICON-A: the atmospheric component of the ICON Earth System Model. Part I: Model description

Giorgetta, M. A., Brokopf, R., Crueger, T., Esch, M., Fiedler, S., Helmert, J., et al. (2018). ICON-A: the atmospheric component of the ICON Earth System Model. Part I: Model description. Journal of Advances in Modeling Earth Systems, 10, 1613-1637. doi:10.1029/2017MS001242.

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Giorgetta, Marco A.1, 2, Autor           
Brokopf, Renate1, 2, Autor           
Crueger, Traute3, 4, Autor           
Esch, Monika1, 2, Autor           
Fiedler, Stephanie4, 5, Autor           
Helmert, J., Autor
Hohenegger, Cathy6, 7, Autor           
Kornblueh, Luis8, Autor           
Köhler, M., Autor
Manzini, Elisa9, Autor           
Mauritsen, Thorsten3, Autor           
Nam, Christine10, Autor           
Raddatz, Thomas11, Autor           
Rast, Sebastian4, 12, Autor           
Reinert, D., Autor
Sakradzija, Mirjana6, Autor           
Schmidt, Hauke4, 12, Autor           
Schneck, Rainer11, Autor
Schnur, Reiner11, Autor           
Silvers, L., Autor
Wan, H., AutorZängl, G., AutorStevens, Bjorn5, Autor            mehr..
Affiliations:
1Climate Modelling, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, ou_913569              
2Wave Driven Circulations, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, Bundesstraße 53, 20146 Hamburg, DE, ou_3001854              
3Climate Dynamics, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, ou_913568              
4Global Circulation and Climate, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, Bundesstraße 53, 20146 Hamburg, DE, ou_3001850              
5Director’s Research Group AES, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, ou_913570              
6Hans Ertel Research Group Clouds and Convection, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, ou_913572              
7Precipitating Convection, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, Bundesstraße 53, 20146 Hamburg, DE, ou_3001851              
8Computational Infrastructure and Model Devlopment (CIMD), Scientific Computing Lab (ScLab), MPI for Meteorology, Max Planck Society, Bundesstraße 53, 20146 Hamburg, DE, ou_2129638              
9Minerva Research Group Stratosphere and Climate, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, ou_2301693              
10The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, ou_913550              
11Global Vegetation Modelling, The Land in the Earth System, MPI for Meteorology, Max Planck Society, ou_913562              
12Middle and Upper Atmosphere, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, ou_913574              

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 Zusammenfassung: ICON‐A is the new icosahedral non‐hydrostatic (ICON) atmospheric general circulation model in a configuration using the Max Planck Institute (MPI) physics package, which originates from the ECHAM6 general circulation model, and has been adapted to account for the changed dynamical core framework. The coupling scheme between dynamics and physics employs a sequential updating by dynamics and physics, and a fixed sequence of the physical processes similar to ECHAM6. To allow a meaningful initial comparison between ICON‐A and the established ECHAM6‐LR model, a setup with similar, low resolution in terms of number of grid points and levels is chosen. The ICON‐A model is tuned on the base of the AMIP experiment aiming primarily at a well balanced top‐of atmosphere energy budget to make the model suitable for coupled climate and Earth system modeling. The tuning addresses firstly the moisture and cloud distribution to achieve the top‐of‐atmosphere energy balance, followed by the tuning of the parameterized dynamic drag aiming at reduced wind errors in the troposphere. The resulting version of ICON‐A has overall biases which are comparable to those of ECHAM6. Problematic specific biases remain in the vertical distribution of clouds and in the stratospheric circulation, where the winter vortices are too weak. Biases in precipitable water and tropospheric temperature are, however, reduced compared to the ECHAM6. ICON‐A will serve as the basis of further development and as the atmosphere component to the coupled model, ICON‐ESM.

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Sprache(n): eng - English
 Datum: 2017-122018-052018-072018-07
 Publikationsstatus: Erschienen
 Seiten: -
 Ort, Verlag, Ausgabe: -
 Inhaltsverzeichnis: -
 Art der Begutachtung: Expertenbegutachtung
 Identifikatoren: DOI: 10.1029/2017MS001242
 Art des Abschluß: -

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Titel: Journal of Advances in Modeling Earth Systems
Genre der Quelle: Zeitschrift
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Seiten: - Band / Heft: 10 Artikelnummer: - Start- / Endseite: 1613 - 1637 Identifikator: -