Escalating High Tide Flooding Along the Atlantic and Gulf Coast of the United States Due To Sea Level Rise

Abstract High tide flooding (HTF) occurs when astronomically driven water levels rise above flooding thresholds in coastal areas, which can happen on sunny days. In a warming climate, sea‐level rise (SLR) is expected to change the frequency of HTF via a direct non‐linear change in the mean water lev...

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Hlavní autoři:	Sadaf Mahmoudi, Hamed Moftakhari, David F. Muñoz, Soheil Radfar, William Sweet, Hamid Moradkhani
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Wiley 2025-09-01
Edice:	Earth's Future
Témata:	sea level rise high tide flooding coastal resilience hydrodynamics modeling
On-line přístup:	https://doi.org/10.1029/2024EF005328
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