Cyclones are important drivers of heat and moisture transport from lower latitudes into the polar regions; they account for nearly three-quarters of the average annual moisture transport into the Arctic (Fearon et al., 2021). The direct thermodynamic impacts of intrusions of warm and moist air in winter are increased downward fluxes of longwave radiation and sensible heat at the snow/ice surface, accompanied by a reduction in sea ice concentration (SIC) (Woods & Caballero, 2016). It has been shown that anomalous warming and moistening triggered by extreme cyclone events can result in near-melting conditions in winter in the Arctic, turn the normally negative surface energy budget (SEB) into a positive one, and thus promote ice melt or reduced ice growth (Boisvert et al., 2016;Moore, 2016;Rinke et al., 2017). But cyclone impacts on Arctic sea ice in winter are not limited to thermodynamics. Cyclone-related wind anomalies lead to a shift of the ice edge position and thus locally reduce or increase the sea ice extent dynamically (Boisvert et al., 2016;Schreiber & Serreze, 2020). Furthermore, ice deformation during storms can promote ice drift divergence and subsequent lead formation and new ice growth as well as ice drift convergence, closing of leads, and formation of pressure ridges (Itkin et al., 2017).Due to these various dynamic and thermodynamic impacts, cyclones are an important driver of Arctic sea ice variability, which plays a key role in the Arctic climate system. Apart from that, the ice edge position and the local SIC are important factors for the marine ecosystem and short-term predictions of both are also crucial for navigation in the Arctic Ocean and its marginal seas. With the climate warming and associated reductions in sea ice thickness and concentration (IPCC, 2021), Arctic navigation is hereby expected to increase in the future (Cao et al., 2022). All this makes it important to understand the impact of cyclones on sea ice. Thereby, the focus of