Abstract
AbstractThe connection between weather extremes and Rossby wave packets (RWP) has been increasingly documented in recent years. RWP propagation and characteristics can modulate the midlatitude weather, setting the scene for temperature and precipitation extremes and controlling the geographical area affected. Several studies on extreme precipitation events (EPEs) in the Alpine area reported, as the main triggering factor, a meridionally elongated upper‐level trough as part of an incoming Rossby wave packet. In this work, we investigate a wide number of EPEs occurring between 1979 and 2015 in northern‐central Italy. The EPEs are subdivided into three categories (Cat1, Cat2, Cat3) according to thermodynamic conditions over the affected region. It is found that the three categories differ not only in terms of the local meteorological conditions, but also in terms of the evolution and properties of precursor RWPs. These differences cannot be solely explained by the apparent seasonality of the flow; therefore, the relevant physical processes in the RWP propagation of each case are further investigated. In particular, we show that RWPs associated with the strongest EPEs, namely the ones falling in Cat2, undergo a substantial amplification over the western North Atlantic due to anomalous ridge‐building 2 days before the event; arguably due to diabatic heating sources. This type of development induces a downstream trough which is highly effective in focusing water vapour transport toward the main orographic barriers of northern‐central Italy and favouring the occurrence of EPEs.
Highlights
Extreme precipitation events (EPEs) in the south-Alpine area are often followed by destructive flooding with severe socio-economic impacts
We show that Rossby wave packets (RWP) associated with the strongest extreme precipitation events (EPEs), namely the ones falling in Category 2 (Cat2), undergo a substantial amplification over the western North Atlantic due to anomalous ridge-building 2 days before the event; arguably due to diabatic heating sources
To further investigate this point, we produce RWP composites based on all EPE cases that occurred in November, a month when both Category 1 (Cat1) and Cat2 EPEs are frequent
Summary
Extreme precipitation events (EPEs) in the south-Alpine area are often followed by destructive flooding with severe socio-economic impacts. The connection between extreme weather events and Rossby wave packets (RWPs) has been documented by many studies that examined the physical linkage between the upper-tropospheric circulation and anomalous weather at the surface. Apart from the presence of a large-scale dynamical forcing factor, Sodemann and Zubler (2010) showed that moisture sources for EPEs in the Alpine area can be distant and pointed to the fact that moisture uptake in the Mediterranean is not the only source. They highlighted the case-to-case variability in this respect.
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