Convection Resolving Climate Simulations



    At present, regional climate models (RCMs) typically use a grid resolution in the order of 10 km to 20 km, at which the convective processes are parameterised. However, with more computational resources becoming available, several groups are investigating the added value of using RCMs on scales, where convection is (partly) resolved by the model (Convection Resolving Climate Simulations; CRCS). This development is driven by the need for kilometer-scale climate information for impact studies (hydrology, wind energy, agriculture, ...), but also by more generic research questions. CRCS are promising research tools for understanding processes and to study feedback mechanisms acting at the local scale (for example feedbacks related to land-atmosphere interactions).

    In the long term, model skill is expected to improve by explicitly resolving the convective processes. Currently, CRCS are at an experimental stage and added value compared to coarser scale climate simulations has only partly been demonstrated yet (e.g., Hohenegger et al., 2008). Conventional evaluation datasets and evaluation methods are not necessarily adequate for evaluating CRCSs and substantial research activity is needed in this domain. Opportunities for using instruments that provide information at small spatial scales (like radar) should be explored. Significant research effort is needed to assess the reliability of CCLM at the convection resolving scale, to identify and trace back its deficiencies, and to support model development.

    Wiki 🔑CECPI-Ger 🔑CECPC5.0🔑Big Brother🔑CRCS_namelist_market🔑CRCS_evaluation_strategy

    Coordinated Evaluation of Convection Permitting Climate simulations with ICON for Germany

    To find optimal parameter settings for predefined model domains a sub-working group is working. The tasks and results are organized via CECPI-Ger (access for CRCS-members only).

    Coordinated Evaluation of Convection Permitting Climate simulations with COSMO-CLM5.0

    To find optimal parameter settings for predefined model domains a sub-working group is working. The tasks and results are organized via wiki (access for CRCS-members only).

    Groups working on CLM_CRCS topics

    Research groups related to CRCS can be found via the topic browser🔑.

    CLM_CRCS related projects

    The CRCS related projects can be found via the topic browser🔑.

    CLM_CRCS Namelist Market

    A marketplace🔑 with namelists that have been used for conducting CRCSs can be found in the Redmine system.

    Please add your namelists to this marketplace, so that modelers who are not that experienced may have a better starting point for their simulations.

    High resolution observational and analysis data

    Wegener Net

    The WegenerNet climate station network region Feldbach comprises 151 meteorological stations in a tightly spaced grid (~ 20 km x 15 km) in the southeastern part of Styria. Temperature, humidity, precipitation, and other parameters are measured with high accuracy and are provided on various temporal scales (from 5 minutes to annual) for both single stations (one station per ~2 km²;) and interpolated regular grids (UTM, 1 km x 1 km; latitude/longitude, 0.01° x 0.01°). For application purposes, all data is available for visualization and download via the WegenerNet data portal ( ).

    Kabas, T., A. Leuprecht, C. Bichler, and G. Kirchengast, WegenerNet climate station network region Feldbach, Austria: network structure, processing system, and example results, Adv. Sci. Res., 6, 49-54, 2011, doi: 10.5194/asr-6-49-2011

    Integrated Nowcasting through Comprehensive Analysis (INCA)

    The Integrated Nowcasting through Comprehensive Analysis (INCA) dataset is produced by the Central Institute for Meteorology and Geodynamics (ZAMG) (Haiden et al. 2011). It has a 1 km × 1 km resolution and covers entire Austria. The INCA dataset is derived via a combination of numerical weather predictions (NWPs) (ALADIN, ECMWF) with current observation data from stations, radar, and satellites, and is further refined with highly resolved orographic information ( ).

    Haiden, T., A. Kann, C. Wittmann, G. Pistotnik, B. Bica, and C. Gruber, The Integrated Nowcasting through Comprehensive Analysis (INCA) System and Its Validation over the Eastern Alpine Region, Wea. Forecasting, 26, 2, 166-183, 2011, doi: 10.1175/2010WAF2222451.1


    Rain gauges and weather radars both constitute important devices for operational precipitation monitoring. Gauges provide accurate yet spotty precipitation estimates, while radars offer high temporal and spatial resolution yet at a limited absolute accuracy. We propose a simple methodology to combine radar and daily rain-gauge data to build

    up a precipitation dataset with hourly resolution covering a climatological time period. The methodology starts from a daily precipitation analysis, derived from a dense rain-gauge network. A sequence of hourly radar analyses is then used to disaggregate the daily analyses. The disaggregation is applied such as to retain the daily precipitation totals of the rain gauge analysis, in order to reduce the impact of quantitative radar biases. Hence, only the radar’s advantage in terms of temporal resolution is exploited. In this article, the disaggregation method is applied to derive a 15-year gridded precipitation dataset at hourly resolution for Switzerland at a spatial resolution of 2 km. Validation of this dataset indicates that errors in hourly intensity and frequency are lower than 25% on average over the Swiss Plateau. In Alpine valleys, however, errors are typically larger due to the shielding effects of the radar and the corresponding underestimation of precipitation

    periods by the disaggregation. For the flatland areas of the Swiss Plateau, the new dataset offers an interesting quantitative description of high-frequency precipitation variations suitable for climatological analyses of heavy events, the evaluation of numerical weather forecasting models and the calibration/operation of hydrological runoff models.

    Wüest, M., C. Frei, A. Altenhoff, M. Hagen, M. Litschi, C. Schär: A gridded hourly precipitation dataset for Switzerland using rain-gauge analysis and radar-based disaggregation, Int J Climatol, 30, 12, 1764–1775, 2010, doi: 10.1002/joc.2025

    The Alpine precipitation grid dataset (EURO4M-APGD)

    MeteoSwiss has developed a gridded analysis of daily precipitation, extending over the entire Alpine region. The dataset is based on measurements at high-resolution rain-gauge networks, encompassing more than 8500 stations from Austria, Croatia, France, Germany, Italy, Slovenia, and Switzerland. The dataset was developed in the framework of EURO4M (European Reanalysis and Observations for Monitoring), a FP7 (seventh framework program) Collaborative Project of the European Union.

    Isotta, F.A. et al. 2014: The climate of daily precipitation in the Alps: development and analysis of a high-resolution grid dataset from pan-Alpine rain-gauge data. Int. J. Climatol., 34: 1657-1675. doi: 10.1002/joc.3794.

    The REGNIE dataset contains daily precipitation on a 1 km grid covering Germany within the period 1961 to 2016 (dataset description ). 

    DWD (2009). Regionalisierte Niederschlagshöhen (REGNIE).

    Der Datensatz "REGNIE" existiert nicht mehr. Er wurde Anfang Januar 2022 durch den "HYRAS-PRE-DE " Datensatz ersetzt.


    Daily precipitation data-set for Sweden on a 4 km grid for 1961 to 2010.

    Johansson, B. (2002). Estimation of areal precipitation for hydrological modelling in Sweden. Ph.D.thesis A76. Earth Science Centre, Göteborg University.


    Daily precipitation and temperature for Norway on a 1 km grid within the period 1957 to 2017. 

    Lussana et al (2019): seNorge_2018 , daily precipitation, and temperature datasets over Norway

    Spain011 (UniCan)

    Daily precipitation on a 0.11° grid for Spain given from 1971 to 2011.

    Herrera, S. et al. (2012). Development and analysis of a 50-year high-resolution daily gridded precipitation dataset over Spain (Spain02)". In: Int. J. Climatol. 32.1, pp. 74-85


    Gridded multiple parameter dataset covering the Carpathian region with 10 km grid spacing from 1961 to 2010.

    Szalai, S. et al. (2013). Climate of the Greater Carpathian Region. Final Technical Report. .

    SAFRAN (Meteo France)

    Gridded reanalysis for France providing multiple sub-daily parameters on an 8 km grid from 1958 to 2013.

    Quintana-Segui, P. et al. (2008). Analysis of near-surface atmospheric variables: Validation of the SAFRAN analysis over France. In: Journal of Applied Meteorology & Climatology 47.1

    A broad buffet of different kinds of observational data can be found under

    • General Observation Period (GOP), covering 2007/2008

    Crewell, S., M. Mech, T. Reinhardt, C. Selbach, H. -. Betz, E. Brocard, G. Dick, E. O'Connor, J. Fischer, T. Hanisch, T. Hauf, A. Hünerbein, L. Delobbe, A. Mathes, G. Peters, H. Wernli, M. Wiegner, and V. Wulfmeyer (2008), The general observation period 2007 within the priority program on quantitative precipitation forecasting: Concept and first results, Meteorol.Z., 17, 6, 849-866, doi: 10.1127/0941-2948/2008/0336 .

    Wulfmeyer, V., A. Behrendt, H. -. Bauer, C. Kottmeier, U. Corsmeier, A. Blyth, G. Craig, U. Schumann, M. Hagen, S. Crewell, P. Di Girolamo, C. Flamant, M. Miller, A. Montani, S. Mobbs, E. Richard, M. W. Rotach, M. Arpagaus, H. Russchenberg, P. Schlüssel, M. König, V. Gärtner, R. Steinacker, M. Dorninger, D. D. Turner, T. Weckwerth, A. Hense, and C. Simmer (2008), RESEARCH CAMPAIGN: The Convective and Orographically Induced Precipitation Study, A Research and Development Project of the World Weather Research Program for Improving Quantitative Precipitation Forecasting in Low-Mountain Regions, Bull.Am.Meteorol.Soc., 89, 10, 1477-1486, doi: 10.1175/2008BAMS2367.1 .

    CLM_CRCS Literature

    Ban, N., J. Schmidli, and C. Schär (2014), Evaluation of the convection-resolving regional climate modeling approach in decade-long simulations, J. Geophys. Res. Atmos., doi:10.1002/2014JD021478

    Chan, S. C., Kendon, E. J., Fowler, H. J., Blenkinsop, S., Roberts, N. M., Ferro, C. A. (2014). The value of high-resolution Met Office regional climate
    models in the simulation of multi-hourly precipitation extremes. Journal of Climate

    Fosser G, Khodayar S, Berg P (2014) Benefit of convection-permitting climate model simulations in the representation of convective precipitation, Climate

    Froidevaux, P., L. Schlemmer, J. Schmidli, W. Langhans, C. Schär (2014): Influence of background wind on the local soil moisture-precipitation feedback. J. Atmos. Sci.,71, 782-799.

    Grell, G. A., L. Schade, R. Knoche, A. Pfeiffer, J Egger (2000): Nonhydrostatic climate simulations of precipitation over complex terrain, J Geophys Res-Atmos.,105 (D24), 29595-29608, doi: 10.1029/2000JD900445

    Hohenegger C., P. Brockhaus, C. Schaer (2008): Towards climate simulations at cloud-resolving scales, Meteorol. Z., 17 (4), 383-394

    P. Brockhaus, C. S. Bretherton and C. Schär (2009): The soil moisture-precipitation feedback in simulations with explicit and parameterized convection, J. Climate , 22 (19), 5003-5020

    Junk, J., A. Matzarakis, A. Ferrone, A. Krein (2014), Evidence of past and future changes in health-related meteorological variables across Luxembourg, Air Qual Atmos Health, 7, 71–81, doi: 10.1007/s11869-013-0229-4

    Kendon, E. J., N. M. Roberts, et al. (2014). "Heavier summer downpours with climate change revealed by weather forecast resolution model." Nature Clim. Change 4(7): 570-576.

    Knote, C., G. Heinemann, B. Rockel, Changes in weather extremes: Assessment of return values using high-resolution climate simulations at convection-resolving scale, Meteorol. Z.19 (1), 11-32, 2010, doi: 10.1127/0941-2948/2010/0424

    Langhans, W., J. Schmidli, C. Schaer: Mesoscale Impacts of Explicit Numerical Diffusion in a Convection-Permitting Model, Mon.Weather Rev., 140(1), 226-244, 2012, doi: 10.1175/2011MWR3650.1

    Langhans, W., J. Schmidli, C. Schaer: Bulk Convergence of Cloud-Resolving Simulations of Moist Convection over Complex Terrain, J. Atmos.Sci., 69(7), 2207-2228, 2012, doi: 10.1175/JAS-D-11-0252.1

    Langhans, W., J. Schmidli, O. Fuhrer, S. Bieri, and C. Schaer (2013): Long-term simulations of thermally driven flows and orographic convection at convection-parameterizing and cloud-resolving resolutions. J. Appl. Meteor. Climatol., 52, 1490-1510.

    Mass, F. C., D. Ovens, K. Westrick, B. A. Colle: Does increasing horizontal resolution produce more skillful forecasts? The results of two years of real-time numerical weather prediction over the Pacific Northwest, B Am Meteorol Soc , 407–430, 2002

    Prein, A. F., and A. Gobiet, NHCM-1: Non-hydrostatic climate modelling. Part I: Defining and Detecting Added Value in Cloud Resolving Climate Simulations, Sci. Rep., 39-2011, 74 pp., 2011, Wegener Center Verlag, Graz, Austria, ISBN 978-3-9502940-6-4, available .

    Prein, A. F., M. Suklitsch, H. Truhetz, and A. Gobiet (2011), NHCM-1: Non-hydrostatic climate modelling. Part III: Evaluation of the LocMIP simulations, Sci. Rep., 41-2011, 128 pp., 2011, Wegener Center Verlag, Graz, Austria, ISBN 978-3-9502940-8-8, avaiable .

    Prein, A. F., A. Gobiet, M. Suklitsch, H. Truhetz, N. K. Awan, K. Keuler, and G. Georgievski (2013) Added Value of Convection Permitting Seasonal Simulations. Clim. Dyn., doi: 10.1007/s00382-013-1744-6 

    Prein, A. F., G. J. Holland, R. M. Rasmussen, J. Done, K. Ikeda, M. P. Clark, and C. H. Liu (2013) Importance of Regional Climate Model Grid Spacing for the Simulation of Precipitation Extremes. J. Climate, doi: 10.1175/JCLI-D-12-00727.1

    Suklitsch, M., A. F. Prein, H. Truhetz, and A. Gobiet, NHCM-1: Non-hydrostatic climate modelling. Part II: Current state of selected cloud-resolving regional climate models and their error characteristics, Sci. Rep., 40-2011, 90 pp., 2011, Wegener Center Verlag, Graz, Austria, ISBN 978-3-9502940-7-1, available

    Tölle, M. H., O. Gutjahr, G. Busch, and J. C. Thiele (2014), Increasing bioenergy production on arable land: Does the regional and local climate respond? Germany as a case study, J. Geophys. Res. Atmos., 119, 2711–2724, doi:10.1002/2013JD020877

    Van Weverberg, K., Goudenhoofdt, E., Blahak, U., Brisson, E., Demuzere, M., Marbaix, P., & van Ypersele, J. P. (2014). Comparison of one-moment and two-moment bulk microphysics for high-resolution climate simulations of intense precipitation. Atmospheric Research, 147, 145-161.

    WG Meetings


    Meeting and Location


    23 Sep 2021

    24th Meeting WG CRCS Assembly, online

    18 March 2021

    Joined meeting of WG CP and CRCS at ICCARUS



    CLM Community Assembly, Lüneburg


    COSMO-CLM User Seminar, Offenbach



    CLM Community Assembly, Belval


    COSMO-CLM User Seminar, Offenbach



    CLM Community Assembly, Frankfurt


    COSMO-CLM User Seminar, Offenbach


    CLM Community Assembly, Zurich


    COSMO-CLM User Seminar, Offenbach


    CLM Community Assembly, Leuven


    COSMO-CLM User Seminar, Offenbach


    CLM Community Assembly, Cava de' Tirreni


    COSMO-CLM User Seminar, Langen


    CLM Community Assembly, Berlin


    CLM Spring meeting, Langen

    WG Annual Reports








    When logged in the link gives the List of WG CRCS members🔑 (without login it shows the complete members list).

    🔑 = Working group members only; CLM-Community login required

    Displaying 0 results.

    Displaying 0 results.

    Displaying results 1..30 of 44.

    Displaying 6 results.

    5th meeting / 2024-06-05 / 13:00-14:30CEST

    Status of ongoing work; discussion of 1st results of CEI100 reference simulations and NUKLEUS CP evaluation simulations; definition of 1st set of test simulations; EVA-Suite development and extensions


    3rd meeting

    Decision on concrete procedures and timelines until mid September, discussion of evaluation procedure


    4th meeting / 2024-05-22

    Reference simulation status, todos, discussion of results CEI100 (tasks from 2nd meeting) and definition of optimisation goals, etc.


    7th meeting / 2024-07-03 / 13:30-15:00CEST

    1. Status ongoing work (efficiency/performance; EVA-Suite improvements/extension; etc.); 2. discussion of first new CEI* sensitivity study results; 3. discussion of configuration option and sensitivity tests (e.g., w.r.t. extreme precipitation bias); 4. definition of test runs; 5. which analysis shall/can be done?; 6. assignment of runs (see CECPI-Ger landing page for links to temporary/planning simulation table)


    6th meeting / 2024-06-19 / 13:30-15:00CEST ***NEW TIME!***

    1. Status ongoing work (efficiency/performance; EVA-Suite improvements/extension; CEI* baseline/reference run(s)); 2. discussion of configuration option and sensitivity tests w.r.t. extreme precipitation bias; definition of test runs; assignment of runs (see CECPI-Ger landing page for links to temporary/planning simulation table)


    8th meeting / 2024-07-17 / 13:30-15:00CEST

    Status ongoing work (efficiency/performance; EVA-Suite improvements/extension; etc.); discussion of ongoing CEI* sensitivity study results; determiniation and assignment of configuration test runs; refinement of the analysis plan (diagnostics and data)

    Agenda and minutes, please edit, comment, or add missing discussion points:

    Zoom meeting room:

    Next meeting: 
    9th meeting / 2024-07-31 / 13:30-15:00CEST -- time might be further adjusted

    Displaying 0 results.

    Displaying 0 results.