Sea Level Rise in the Samoan Islands Escalated by Viscoelastic Relaxation After the 2009 Samoa-Tonga Earthquake

Following the 2009 Samoa-Tonga earthquake, the Samoan islands, including Savai'i, Upolu, and Tutuila, have experienced accelerated sea-level rise, driven by subsidence and gravity changes, with American Samoa witnessing a 5 times faster rate than the global average. A viscoelastic model predicts a continued sea-level rise of 30-40 cm, intensifying coastal flooding.