Multi-day hail clusters and isolated hail days in Switzerland – large-scale flow conditions and precursors

نویسندگان

چکیده

Abstract. In Switzerland, hail regularly occurs in multi-day clusters. The atmospheric conditions prior to and during clusters are described contrasted the isolated days. analysis focuses on days that occurred between April September 2002–2019 within 140 km of Swiss radar network. Hail north south Alps defined using a minimum area threshold radar-based product. Multi-day as 5 d windows containing 4 or single day. reanalysis ERA-5 is used study large-scale flow combination with objectively identified cold fronts, blocking events, weather type classification. Both Alps, have frequency maxima May August–September, whereas clustered occur mostly July August. Composites variables indicate more stationary meridionally amplified both On blocks frequent over North Sea, surface fronts located farther from Switzerland than Clustered also characterized by significantly higher most unstable convective available potential energy (MUCAPE) values, warmer daily maximum temperatures, moisture content Hence, anomalous amounts necessary for side. contrast, differences MUCAPE side small. mean sea level pressure deeper, temperature colder, local lower upper-level eastern Atlantic 3 Moreover, 10 % Scandinavia, but no Half Alps. clustering only frequently Alpine ridge, low-level winds stronger. temporal coupled specific synoptic- local-scale conditions; this information may be exploited short- medium-range forecasts Switzerland.

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ژورنال

عنوان ژورنال: Weather and climate dynamics

سال: 2021

ISSN: ['2698-4016']

DOI: https://doi.org/10.5194/wcd-2-1167-2021