Model projections show a more or less rapid continuation of this ongoing process depending on the greenhouse gas emission scenario, with likely summer ice-free Arctic conditions (September Arctic sea-ice area lower than 1 million km 2 ) occurring before 2050 (Arthun et al., 2021; SIMIP Community, 2020).Recent changes in Arctic sea ice have been linked to both anthropogenic global warming (Notz & Stroeve, 2016) and climate internal variability (Swart et al., 2015). However, the exact drivers influencing sea-ice loss and their respective contributions are not fully understood. Both atmospheric (Ding et al., 2017) and ocean (Carmack et al., 2015) processes play a role in Arctic sea-ice changes. Typically, changes in near-surface air temperature strongly control the variability in Arctic sea-ice area over short time scales (Olonscheck et al., 2019), while ocean heat transport has a stronger impact on longer time scales (Onarheim et al., 2015).The influence of atmospheric and ocean processes on Arctic sea ice is usually quantified via correlation and regression analyses, including or not a lag (