Extreme precipitation events over northern Italy. Part II: Dynamical precursors

• Published in: Quarterly Journal of the Royal Meteorological Society
• Main Authors: Grazzini, Federico, Fragkoulidis, Georgios, Teubler, Franziska, Wirth, Volkmar, Craig, George C., 3 Institute for Atmospheric Physics, Johannes Gutenberg University Mainz Mainz Germany, 1 Ludwig‐Maximilians‐Universität, Meteorologisches Institut Munich Germany
• Format: Article in Journal/Newspaper
• Language: English
• Published: John Wiley & Sons, Ltd. 2021
• Subjects: ddc:551.6; atmospheric rivers; extreme precipitation; integrated water vapour transport; large‐scale forcing; potential vorticity; Rossby wave packets; North Atlantic
• Online Access: https://doi.org/10.1002/qj.3969; http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/8420

The 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. The EPEs are subdivided into three categories (Cat1, Cat2, Cat3) according to thermodynamic conditions over the affected region. The three categories not only differ locally but also in the evolution of precursor RWPs as visible in the composite Hovmöller plots. RWPs associated with the strongest EPEs, the ones falling in Cat2, undergo a substantial amplification over the west North Atlantic due to anomalous ridge‐building 2 days before the event. ...