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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, Author                 
Brokopf, Renate1, 2, Author           
Crueger, Traute3, 4, Author           
Esch, Monika1, 2, Author           
Fiedler, Stephanie4, 5, Author           
Helmert, J., Author
Hohenegger, Cathy6, 7, Author           
Kornblueh, Luis8, Author           
Köhler, M., Author
Manzini, Elisa9, Author                 
Mauritsen, Thorsten3, Author           
Nam, Christine10, Author           
Raddatz, Thomas11, Author           
Rast, Sebastian4, 12, Author           
Reinert, D., Author
Sakradzija, Mirjana6, Author           
Schmidt, Hauke4, 12, Author                 
Schneck, Rainer11, Author
Schnur, Reiner11, Author                 
Silvers, L., Author
Wan, H., AuthorZängl, G., AuthorStevens, Bjorn5, Author                  more..
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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 Abstract: 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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Language(s): eng - English
 Dates: 2017-122018-052018-072018-07
 Publication Status: Issued
 Pages: -
 Publishing info: -
 Table of Contents: -
 Rev. Type: Peer
 Identifiers: DOI: 10.1029/2017MS001242
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Title: Journal of Advances in Modeling Earth Systems
Source Genre: Journal
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Pages: - Volume / Issue: 10 Sequence Number: - Start / End Page: 1613 - 1637 Identifier: -