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Convection Resolving Climate Simulations

WG CRCS

Coordinators

Andreas Will (BTU)

Co-Coordinator: Klaus Görgen (FZJ)

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

Overview

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.

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 (www.wegenernet.org ).

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 (http://www.zamg.ac.at/forschung/synoptik/inca/ ).

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

CH02H

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)

doi:10.18751/Climate/Griddata/APGD/1.0
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.

REGNIE (DWD)
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.

PTHBV (SMHI)

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.

KLIMAGRID (met.no)

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

CARPATCLIM

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. www.carpatclim-eu.org .

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
Dynamics

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

Date

Meeting and Location

Documents

23 Sep 2021

24th Meeting WG CRCS Assembly, online

18 March 2021

Joined meeting of WG CP and CRCS at ICCARUS

🔑Minutes

2016

CLM Community Assembly, Lüneburg

2016

COSMO-CLM User Seminar, Offenbach

🔑Minutes

2015

CLM Community Assembly, Belval

2015

COSMO-CLM User Seminar, Offenbach

🔑Minutes

2014

CLM Community Assembly, Frankfurt

2014

COSMO-CLM User Seminar, Offenbach

2013

CLM Community Assembly, Zurich

2013

COSMO-CLM User Seminar, Offenbach

2012

CLM Community Assembly, Leuven

2012

COSMO-CLM User Seminar, Offenbach

2011

CLM Community Assembly, Cava de' Tirreni

2011

COSMO-CLM User Seminar, Langen

2010

CLM Community Assembly, Berlin

2010

CLM Spring meeting, Langen

WG Annual Reports

WG_CRCS_Annual_Report_2011.pdf

WG_CRCS_Annual_Report_2012.pdf

WG_CRCS_Annual_Report_2013.pdf

WG_CRCS_Annual_Report_2014.pdf

WG_CRCS_Annual_Report_2015.pdf

WG_CRCS_Annual_Report_2016.pdf

Members

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

The aim of application of Regional Climate Models (RCMs) is to provide reliable informaion about climate and climate change on regional to local scales. The need for climate change results on convection resolving scale is increasing. RCMs based on non-hydrostatic models of the atmosphere can simulate the climate on grid scales down to 1 km, at which convective processes are partly to fully resolved. Due to limited computational resources the grid resolution and simulation domain vary substantially in Convection Resolving Climate Simulations (CRCS). The effective model resolution of the simulations is significantly smaller than the grid size, parameters describing the land scape have limited quality and/or resolution, and there is still a need for parameterisation of unresolved processes. This makes the set-up and the fidelity of the models dependent on the simulated region and domain of application. The added value, compared to coarser scale climate simulations, has only partly been demonstrated. The relevance of several processes for climate variability on local scales is unknown. High resolution observations are available for very few quantities only and not everywhere. The quality of simulated climate variability on regional to local scales is thus partly unknown and/or requires further improvement. Also, the quality of results is partly insufficient for usage in climate impact studies and makes a bias correction necessary. Hence, there is a need for coordinated research and development efforts: (i) on the development of generic km-scale climate model set-ups for long climate simulations, including specific parameterisations of regional and local effects (with relevance, e.g., for hydrology, renewable energy, agriculture, etc.); (ii) for further evaluation data and evaluation methods appropriate for CRCS simulations; (iii) for a be?er understanding of processes, mechanisms and variability of regional to local climate; (iv) to reduce model structural deficiencies, and to support model development. The working group is a pla`orm for discussion and collaboration on these aspects. The WG collaborates with other WGs in the CLM-Community and with national and international initiatives on convection resolving modelling.

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