The images and animations presented below show a case of well-organised convection over the Western Mediterranean Sea. The unstable situation lasted for at least three days (14-16 October 2003) with rapidly developing storms occurring over Tunesia, Southern Italy and Spain (Balearic Islands). The most severe storms occurred on 15 October over the Mediterranean Sea close to Sicily, and on 16 October in the area of the Balearic Islands. In the first case, a long-lived storm with a well-developed flanking line developed within warm unstable air that had been pushed into this area by an upper-level low situated over the Balearic Islands. This storm, which reached cloud top temperatures of about -65°C, showed a V-shape with an area of higher cloud top temperatures to the lee of the overshooting top (see colour-enhanced IR10.8 image). The V-shape structure indicates with high probability that this storm was associated with severe weather phenomena (see also Storm over Hamburg on 9 June 2004). In the second case, a series of severe storms developed over and around the Balearic Islands.
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The images below show some Nowcasting products based on Meteosat-8
data that have been generated by the Nowcasting
SAF. The top two images show the cloud type and the cloud top pressure
products (at SEVIRI pixel resolution), which help the forecaster to carry
outa detailed cloud analysis without having to look at the individual channels
of Meteosat-8.
The bottom two images show the Automatic Satellite Image
Interpretation (ASII) and the Rapidly Developing Storms (RDT) products
(from the previous day), which are based on a textural and temporal analysis
of the Meteosat-8 images (mainly the IR10.8 channel). The aim of the ASII
product is an automatic image interpretation in terms of conceptual models
(CM). A CM analysis can be used for detailed synoptic diagnosis and for
the early detection of ongoing meteorological processes, as well as for
the determination of the stage of development of these processes. The
RDT product is intended to provide the forecaster with information about
significant convective systems from storm-scale up to meso-alpha scale.
It also helps to identify, track and monitor intense convective systems
and rapidly developing convective cells.
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