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- W2070963546 abstract "Rain-producing flows over the south side of the Alps are investigated with an idealized high-resolution (2.5 km) numerical configuration where only three basic ingredients of typical heavy-precipitation situations have been retained: (1) a uniform and stationary southerly flow far upstream from the Alps, which drives (2) a conditionally unstable atmosphere towards (3) the real topography of the Alps and the surrounding secondary mountains. Attention is given to small-scale mechanisms of rainfall over the Po Plain and the Alpine slopes. These are linked with two orographically induced low-level wind jets: the easterly barrier-wind jet along the southern flank of the Alps and a south-easterly jet formed over the sea along the south-western flank of the Apennines and continuing over land up to the Alps. The specific role of the secondary relief upstream from the Alps in inducing or influencing these low-level flow features, and also in triggering organized convection, is studied by means of experiments on the sensitivity to topography. The idealized configuration also allows the advantages of a convection-resolving model for modelling precipitation distributions at the Alpine valley scale to be considered. Copyright © 2007 Royal Meteorological Society" @default.
- W2070963546 created "2016-06-24" @default.
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- W2070963546 date "2003-04-16" @default.
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- W2070963546 title "Small-scale rainfall mechanisms for an idealized convective southerly flow over the Alps" @default.
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- W2070963546 doi "https://doi.org/10.1256/qj.02.85" @default.
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