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- W2016173314 abstract "Storms have been traditionally based on anemometric excesses. We argue you here a different point of view, one where isobaric developments are also taken into balance. As a result, a storm hecomes a single individual entity, that is an aggravated low pressure. That explains why the physionomical features are privileging the trajectories and their related barometric developments. In order to explain sudden aggravations, we show that the aggravation process depends on the warm air-mass entering into the talwegs. This phenomenon can take place during the Fall when strong warm advections swarmed into the the higher talwegs, which are being deformed on the midst of huge low geopotential zones. During the Winter, with the renewed situation of quick zonal circulations, sudden deformations in the upper-jet are putting into palce in Europe's Western coast clear spatialized geopotential drops. These moving talwegs still cause violent risings of warm air-mass. Least expected during Winter, this mechanism remains hazardous." @default.
- W2016173314 created "2016-06-24" @default.
- W2016173314 creator A5033688735 @default.
- W2016173314 date "2003-01-01" @default.
- W2016173314 modified "2023-09-25" @default.
- W2016173314 title "Les tempêtes, un concept et une genèse revisités : I'exemple de la façade occidentale de l'Europe / Storms, a notion revisitated : the case of Western Europe facade" @default.
- W2016173314 cites W1969921266 @default.
- W2016173314 doi "https://doi.org/10.3406/geo.2003.963" @default.
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