Climatological aspects of quasi-linear convective systems across Europe

Abstract

<p>In this work, we use 8 years of OPERA radar data, ESWD severe weather reports, and ATDnet lightning detection data to create a climatology of quasi-linear convective systems (QLCS) across Europe. In the first step, 15-minute composite animations of radar reflectivity and lightning data were used to manually identify 2201 QLCS polygons in the period of 2014 to 2021. Severe weather reports, lightning data, and morphological properties (such as the presence of bowing segments) allowed classifying QLCSs according to their intensity into 1844 marginal, 304 moderate, and 53 derecho cases. The manual evaluation also allowed us to identify: the basic archetype of the system, the location of stratiform precipitation relative to the active convective part, propagation with respect to the mean wind, areal coverage, width, length, accompanying hazards, and social impacts associated with each QLCS. Results indicate that QLCSs are the most frequent during summer in Central Europe, while in southern Europe the season of their occurrence is extended to late autumn. QLCSs are the least frequent during winter when they appear mostly in northwestern Europe in the form of narrow cold frontal rainbands (NCFR). In spring they are most common across western Europe. The vast majority of systems move from southwest and west. 22% of the systems were associated with a bow echo signature and 6% produced a mesoscale convective vortex. Among precipitation modes, trailing (53%) and embedded (45%) stratiform types were the most common. The longest classified QLCS had a length of 2200 km (9 Aug 2018), while the widest reached 1635 km (10 Jan 2015). The most frequent hazard accompanying QLCSs was lightning (produced during 95% of the total QLCSs lifetime), followed by severe winds gusts (7.7%), excessive precipitation (5.3%), large hail (2.7%), and tornadoes (0.4%). Derechos had the largest coverage of severe wind reports with respect to their path area (49%), while back-building QLCS had the largest coverage of excessive precipitation events (12%). Large hail was most common with bow-echo complexes (6.5%).</p>

The characteristics of mesoscale convective system rainfall over Europe

“…range in their western parts (Tibetan Plateau and Andes, respectively) and thus feature similar topographic characteristics as the midwest USA. Conversely, the varied European topography with several mountain ranges oriented along different directions might make for a more complex picture of the MCS diurnal cycle.Focusing on a restricted part of EuropeSurowiecki & Taszarek, 2020), investigating only one season, or using a limited time record to assess climatological properties, several studies have examined MCS over Europe. Using five years of infrared (IR) satellite data, found that summer MCS (April-September) are more common over land than sea and are triggered near mountainous areas (Pyrenees, Alps, Carpathians) during the afternoon, a general characteristic also found for the USA.The present study composes a comprehensive MCS rainfall climatology over Europe from 16 years of the Integrated Multi-satellitE Retrievals for GPM (IMERG) combined with EUropean Cooperation for LIghtning Detection (EUCLID) lightning data.…”