;
Luna Rico, María Yolanda
[3]
;
González-Alemán, Juan Jesús
[3]
;
Sastre, Mariano
[1]
;
Valero, Francisco
[1]
;
Farrán, José Ignacio
[2]
;
Martín, María Luisa
[2]
Madrid, España
Valladolid, España
Madrid, España
Supercells are a type of severe convective storms usually associated with adverse meteorological phenomena (large hail, strong winds, thunderstorms, floods, tornadoes...). These phenomena can be extremely destructive and cause a great deal of material damage and occasionally personal injuries. Therefore, it is important to study supercells in detail to achieve a correct forecast and anticipate possible consequences. In this paper, a supercell event occurred in eastern Spain on 31 July 2015 is presented. The event caused great destruction in several locations due to strong winds and large hail (greater than 8 cm diameter). The system was simulated with the Weather Research and Forecasting (WRF-ARW) model. The synoptic situation was characterized by the presence of a deep trough whose axis was located over the Iberian Peninsula, promoting positive vorticity and divergence advection to occur in front of the axis, providing a favorable convective environment for the supercells development. The MSG-SEVIRI satellite brightness temperature (10.8 µm infrared channel) is used as a meteorological variable to validate and compare the simulations of the cloudiness associated with the supercell event. The validation of the WRF model is performed thorough several skill-scores, giving satisfactory results in the distribution of the brightness temperature of the supercells with a slight overestimation of it.
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