SKIRON/Eta system with dust capabilities – Quick description The SKIRON/Eta system is based on the Eta/NCEP limited area atmospheric model developed at the University of Athens, Atmospheric Modeling and Weather Forecasting Group - UOA/AM&WFG, Kallos et al, (1997). Its major parts of the system are the modified Eta/NCEP atmospheric model and the dust cycle modules. The Eta model is well-documented and detailed descriptions of its dynamics and physics components can be found in several studies (e.g., Mesinger et al., 1988; Janjic, 1994, and references therein). The modifications and improvements incorporated in the atmospheric model are these suggested by the SKIRON and POSEIDON projects, especially in the parameterizations of the atmospheric radiation and surface processes (Kallos et al., 1997; Papadopoulos et al., 1997, 2002). The dust modules (Dust REgional Atmospheric Model - DREAM) were developed and tested also at the UOA/AM&WFG, in the framework of the MEDUSE project (Kallos et al., 1997, Nickovic et al., 1997). The integrated system has been further developed in the framework of ADIOS Project and the current model version incorporates state-of-the-art parameterizations of all the major phases of the atmospheric dust lifecycle such as production, diffusion, advection, and removal, including as well the effects of the particle size distribution on aerosol dispersion and deposition. In this version of the model, four size bins were considered with centered diameters of 1.5, 12, 36, and 76 μm as suggested by Tegen and Fung (1994). A detailed description of the dust cycle module is given in the work of Nickovic et al., (2001). The system has evaluated by utilizing various types of observations for specific episodes as well as for longer periods. Evaluation of the system has performed over the Mediterranean Sea and Atlantic Ocean (Kallos et al., 2006), the Iberian Peninsula by Rodriguez et al. (2001) and Escudero (2006). Older versions of the system were used to perform studies of historical dust-storm events (Kubilay et al., 2000; Tsidulko et al., 2002). The SKRON/Eta system (same atmospheric and dust prediction system) was in operation in Malta under the name of the dust module - DREAM. This operational version of the SKIRON/Eta system has evaluated by comparing its forecasts with lidar observations in the framework of the EARLINET project (Balis et al. 2006) and surface observations (Kallos et al., 2006). Recently, the same system is in use in Barcelona where further development concerning the radiative transfer scheme was performed (Perez et al. 2006). References Balis, D., and Coauthors, 2006: Optical characteristics of desert dust over the East Mediterranean during summer: a case study. Annales Geophysicae, 24, 807-821. Escudero, M., 2006: Suspended particulate matter and wet deposition fluxes in regional background areas of the Iberian Peninsula. PhD Thesis, University of Barcelona, February 2006. Janjic, Z.I. (1994), The step-mountain eta coordinate model: further developments of the convection, viscous sublayer and turbulence closure schemes, Mon. Weather Rev., 122, 927-945. Kallos, G., S. Nickovic, D. Jovic, O. Kakaliagou, A. Papadopoulos, N. Misirlis, L. Boukas, N. Mimikou, G. Sakellaridis, J. Papageorgiou, E. Anadranistakis, M. Manousakis, (1997), The Regional Weather Forecasting System SKIRON and its capability for forecasting dust uptake and transport. Proceedings of the WMO conference on dust storms, 6 November 1997, Damascus, Syria. Kallos, G., S. Nickovic, A. Papadopoulos, D. Jovic, O. Kakaliagou, N. Misirlis, L. Boukas, N. Mimikou, G. Sakellaridis, J. Papageorgiou, E. Anadranistakis, and M. Manousakis (1997), The regional weather forecasting system SKIRON: An overview, paper presented at the International Symposium on Regional Weather Prediction on Parallel Computer Environments, University of Athens, Athens, Greece, 15-17 October 1997. Kallos, G., A. Papadopoulos, P. Katsafados, and S. Nickovic (2006), Trans-Atlantic Saharan dust transport: Model simulation and results. J. Geophys. Res., 111, doi:10.1029/2005JD006207. Kubilay, N., S. Nickovic, C. Moulin, and F. Dulac (2000), An illustration of the transport and deposition of mineral dust onto the eastern Mediterranean, Atmos. Environ., 34, 1293-1303. Mesinger, F., Z.I. Janjic, S. Nickovic, D. Gavrilov and D.G. Deaven (1988), The steepmountain coordinate: Model description and performance for cases of Alpine lee cyclogenesis and for a case of an Appalachian redevelopment, Mon. Weather Rev., 116, 1493-1518. Nickovic, S., D. Jovic, O. Kakaliagou, and G. Kallos (1997), Production and long-range transport of desert dust in the Mediterranean region: Eta model simulations, paper presented at 22nd NATO/CCMS International Technical Meeting on Air Pollution Modeling and Its Applications, Clermont-Ferrand, France, 2-6 June 1997. Nickovic, S., G. Kallos, A. Papadopoulos and O. Kakaliagou (2001), A model for prediction of desert dust cycle in the atmosphere. J. Geophys. Res., 106, 18113-18129. Papadopoulos, A., G. Kallos, S. Nickovic, D. Jovic, M. Dacic, and P. Katsafados (1997), Sensitivity studies of the surface and radiation parameterization schemes of the Skiron system, paper presented at the International Symposium on Regional Weather Prediction on Parallel Computer Environments, University of Athens, Athens, Greece, 15-17 October 1997. Papadopoulos, A., G. Kallos, P. Katsafados, and S. Nickovic (2002), The POSEIDON weather forecasting system: An overview, The Global Atmosphere and Ocean Systems, 8, 219-237. Perez, C., S. Nickovic, J. M. Baldasano, M. Sicard, F. Rocadenbosch and V. E. Cachorro (2006) A long Saharan dust event over the western Mediterranean: Lidar, Sun photometer observations, and regional dust modeling. J. Geophys. Res., 111, doi:10.1029/2005JD006579. Rodriguez, S., X. Querol, A. Alastuey, G. Kallos, and O. Kakaliagou (2001), Saharan dust inputs to suspended particles time series (PM10 and TSP) in Southern and Eastern Spain. Atmos. Environ., 35, 2433-2447. Tegen, I., and I. Fung (1994), Modeling of mineral dust in the atmosphere: Sources, transport and optical thickness, J. Geophys. Res., 99, 22897-22914. Tsidulko, M., S.O. Krichak, P. Alpert, O. Kakaliagou, G. Kallos, and A. Papadopoulos (2002), Numerical study of a very intensive eastern Mediterranean dust storm, 13-6 March 1998, J. Geophys. Res., 107(D21), 4581, doi:10.1029/2001JD00168.