A 45-month EDR measurement archive (2019-2022) is employed in this study as the observational CAT database and around 5000 events with moderate or greater (MoG) intensity are identified. The observed events are analyzed together with synoptic weather systems affecting the tropopause region, which are identified with feature-based methods in the ERA5 reanalysis. While the jet stream showed a high frequency of co-occurrence with CAT, Rossby wave breaking (RWB; using potential vorticity streamers as a proxy) and warm conveyor belt (WCB) ascent are also frequently concurrent with the CAT events. A categorization of the events with respect to these two weather systems shows that they account for around 70% of the observed events and the very different properties of the two categories are revealed, with high horizontal deformation associated with the RWB-concurrent events and higher frequency of negative potential vorticity being present in the vicinity of the WCB-concurrent events. Deformation and the diabatic processes related to WCBs are hence suggested to be potential triggering processes of these two types of CAT.
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