Bueno como muchos aqui,miras modelos y te vuelves loco sobre lo que va a pasar a partir de mañana,entre choque de masas y posibles borrascas profundisimas con posibilidad de ciclogenesis en andalucia,entones hago un pequeño resumen de lo que empiezan a ver los diferentes modelos a nivel de alarmas y avisos:
Avisos Aemet:
Viernes:Cordoba,Sevilla,Huelva,Cadiz y Ceuta alerta amarilla por lluvias 15 mm/h
Sabado:Cordoba,Sevilla,Cadiz y Ceuta,alerta amarilla por lluvias 15mm/h y fenomenos costeros en Huelva,Cadiz y Ceuta.
STOFEX:
Strait of Gibraltar, S-Portugal, extreme SW-Spain and N-Morocco ...
The ingredients seem to come together for a major freezing rain/snow event over south/central Spain! In respect of convection, elevated thunderstorms can't be ruled out well inland of S-Spain, which would locally increase the heavy (freezing) rain and snow risk significantly.
During the daytime hours, the active arctic front pushes southwards, reaching S Portugal/Spain during the late night hours. At the same time, a vigorous depression off the Azores keeps moving eastwards while filling. Due to the low latitude of this depression, the warm sector is filled with true tropical air mass and persistent influx of this very moist air continues during the forecast. Isolated to scattered thunderstorms are possible in the warm sector mainly west of the Strait of Gibraltar during the daytime hours due to the weakly capped airmass and very moist BL, but overall thunderstorm coverage is on the increase during the night, as the arctic front at the surface approaches the strait from the north. Shear is not that strong and multicells are the primary storm mode. Clustering of those storms is likely with some upper divergence overspreading the area from the west with an excessive rain risk. An isolated tornado/waterspout risk can't be excluded mainly west of the Strait of Gibraltar, as LL CAPE increases. Despite the signals of high rain amounts, the coverage of storms in this (sub) tropical airmass could be not as widespread as expected by models due to the clustering of storms and the evolution of a more stratiform rain field with embedded, convective elements. We therefore went with a high-end level 1 for excessive rain.
A low probability thunderstorm area was issued well inland, as some MUCAPE atop of the surface cold front may yield an adequate environment for isolated thunderstorms. These storms may pose an increased risk for sleet, marginal hail and freezing rain, as WBZ lowers.
Eso junto al mapa de spainsevereweather parece que esta claro del riesgo que se nos viene encima....
SI alguien puede traducir el texto de estofex,hay pronostica todo lo que va a pasar...el choque de masas