Title of article :
The 14 July 2001 hailstorm in northeastern Spain: diagnosis of the meteorological situation
Author/Authors :
Tudur??، نويسنده , , E and Romero، نويسنده , , R and L?pez، نويسنده , , L and Garc??a، نويسنده , , E and S?nchez، نويسنده , , J.L and Ramis، نويسنده , , C، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2003
Abstract :
Hail producing thunderstorms developed over the Ebro valley (NE Spain) during the evening of 14 July 2001, affecting mainly the Lerida province. Hail stones as large as 3 cm in diameter produced damage on 2979 ha of fruit trees, vineyard and cornfields. The thunderstorms developed ahead of a cold front, which was moving from the Gulf of Biscay towards inland Spain. Meteosat images and radar data demonstrate that the storms formed over the central part of the Ebro valley and moved towards the east attaining their maximum development in Lerida province. A diagnosis, using data from ECMWF, shows that at surface there was a cyclonic circulation over northeastern Spain and at medium levels (500 hPa) a trough with cold air located towards northwestern Spain. The Q vector diagnosis demonstrates that the forcing for upward vertical motions was rather weak at both low and medium levels over the area where the thunderstorms developed. However, a significant frontogenesis contribution is identified over the Ebro valley. A more detailed handmade analysis shows that over the Ebro valley there was a thermal mesolow, which favoured the inland entrance of humid air from the Mediterranean. Frontogenesis and the humid air intrusion coexisted where remote-sensing observations indicated that the storms developed. A numerical study of the event using the MM5 model has been carried out. In a control experiment, the model is able to develop the thermal mesolow and reproduce, quite well, the convergence produced by the front as well as the timing of the event. In order to study the genesis and influence of the thermal mesolow, another simulation has been performed without consideration of solar radiation. The results indicate that the thermal mesolow does not develop, the convergence ahead of the cold front is significantly weakened and the front itself becomes increasingly progressive. As a result, thunderstorms do not develop and very little precipitation falls in the area.
Keywords :
Thunderstorm , hail , Remote sensing
Journal title :
Atmospheric Research
Journal title :
Atmospheric Research