Nearshore bathymetric changes along the Alaska Beaufort Sea coast and possible physical drivers

• Published in: Continental shelf research 2022-06, Vol.242, p.104745, Article 104745
• Main Authors: Zimmermann, Mark, Erikson, Li H., Gibbs, Ann E., Prescott, Megan M., Escarzaga, Stephen M., Tweedie, Craig E., Kasper, Jeremy L., Duvoy, Paul X.
• Format: Article
• Language: English
• ISSN: 0278-4343; 1873-6955
• DOI: 10.1016/j.csr.2022.104745

Erosion rates along Alaska's Beaufort Sea coast, among the highest in the world, are negatively impacting communities, industrial and military infrastructure, and wildlife habitat. Decreasing maximal winter ice extent and increasing summer open water duration and extent in the Beaufort Sea may be making the coast more vulnerable to destructive storm waves than during recent, colder, icier decades. Previous studies of Beaufort Sea coastal change have been limited to subaerial analyses of the shoreline. Here we describe nearshore seafloor change by comparing post-World War II (WWII) (1945-53) bathymetry data to recently acquired (1985–2018) bathymetry data and relate the observed seafloor change to adjacent shoreline change near Utqiagvik, within Stefansson Sound, and immediately west of Barter Island and Kaktovik. Within the Utqiagvik region, seabed erosion was generally highest (>1.0 m of loss) offshore of Point Barrow and along the eastern end of the Tapkaluk Islands, while there were lesser amounts of deposition (