“…The functioning of the present‐day Arctic coastal system is also influenced by permafrost degradation (e.g., Wobus et al, ), storm‐surge floodings (e.g., Pisaric et al, ), increased sediment supply from glacial catchments (e.g., Mercier & Laffly, ), and even such extreme events as tsunamis (e.g., Buchwał, Szczuciński, Strzelecki, & Long, ; Dahl‐Jensen et al, ; Long, Szczuciński, & Lawrence, ). Majority of those changes have a strong impact on circum‐polar Arctic coastal communities and their historical (including archaeological) and modern infrastructure (e.g., Ford, Bell, & St‐Hilaire‐Gravel, ; Gorokhovich, Leiserowitz, & Dugan, ; Hatcher & Forbes, ; Mason, Jordan, Lestak, & Manley, ; Radosavljevic et al, ).…”