Abstract
Abstract. For the first time, the Limited-Area Mode of the new ICON (Icosahedral Nonhydrostatic) weather and climate model has been used for a continuous long-term regional climate simulation over Europe. Built upon the Limited-Area Mode of ICON (ICON-LAM), ICON-CLM (ICON in Climate Limited-area Mode, hereafter ICON-CLM, available in ICON release version 2.6.1) is an adaptation for climate applications. A first version of ICON-CLM is now available and has already been integrated into a starter package (ICON-CLM_SP_beta1). The starter package provides users with a technical infrastructure that facilitates long-term simulations as well as model evaluation and test routines. ICON-CLM and ICON-CLM_SP were successfully installed and tested on two different computing systems. Tests with different domain decompositions showed bit-identical results, and no systematic outstanding differences were found in the results with different model time steps. ICON-CLM was also able to reproduce the large-scale atmospheric information from the global driving model. Comparison was done between ICON-CLM and the COnsortium for Small-scale MOdeling (COSMO)-CLM (the recommended model configuration by the CLM-Community) performance. For that, an evaluation run of ICON-CLM with ERA-Interim boundary conditions was carried out with the setup similar to the COSMO-CLM recommended optimal setup. ICON-CLM results showed biases in the same range as those of COSMO-CLM for all evaluated surface variables. While this COSMO-CLM simulation was carried out with the latest model version which has been developed and was carefully tuned for climate simulations on the European domain, ICON-CLM was not tuned yet. Nevertheless, ICON-CLM showed a better performance for air temperature and its daily extremes, and slightly better performance for total cloud cover. For precipitation and mean sea level pressure, COSMO-CLM was closer to observations than ICON-CLM. However, as ICON-CLM is still in the early stage of development, there is still much room for improvement.
Highlights
Background informationIn 1999, the limited-area weather forecast model LM (Lokalmodell, Doms and Schättler, 1999; later COnsortium for Small-scale MOdeling (COSMO), Baldauf et al, 2011), which was developed by the Deutscher Wetterdienst (DWD, the German Meteorological Service), became operational together with the “Global-Modell” (GME) global model (Majewski and Ritter, 2002)
A few years later, it was renamed into the “COSMO model” in order to reflect that further development has become a joint task of the COnsortium for Small-scale MOdeling (COSMO)
The new ICON-CLM regional climate model has been derived from the ICON-Limited-Area Mode (LAM) weather forecast model along with the necessary technical infrastructure and evaluation tools, allowing users to carry out and evaluate long-term regional climate simulations
Summary
In 1999, the limited-area weather forecast model LM (Lokalmodell, Doms and Schättler, 1999; later COSMO, Baldauf et al, 2011), which was developed by the Deutscher Wetterdienst (DWD, the German Meteorological Service), became operational together with the “Global-Modell” (GME) global model (Majewski and Ritter, 2002). A few years later, it was renamed into the “COSMO model” in order to reflect that further development has become a joint task of the COnsortium for Small-scale MOdeling (COSMO). In 2002, the Climate Limited-area Modeling Community (CLM-Community) developed the first version of the regional climate model named CLM. In 2007, the developments in COSMO and CLM were recombined and a first unified version of the weather forecast and climate modes, named COSMO-CLM (Rockel et al, 2008), was released.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.