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Human-Caused Sea Level Rise Is Driving a Global Surge in Coastal Flooding

The studies show greenhouse-gas driven warming has already made once-rare coastal floods far more common, forcing a rethink of flood planning and emissions choices.

FILE - Waves lap the beach where remains of Afeli Bernice Adzo's family home stand after it was destroyed by coastal erosion in Avegadzi, Ghana, March 5, 2025 (AP Photo/Misper Apawu, File)
FILE - Cars and debris from washed away homes line a canal in Fort Myers Beach, Fla., Oct. 5, 2022, one week after the passage of Hurricane Ian. (AP Photo/Rebecca Blackwell, File)
FILE - People wade through a recreational vehicle park flooded by a king tide on Jan. 3, 2026, near Corte Madera in Marin County, Calif. (AP Photo/Ethan Swope, File)
FILE - People recover belongings from a home flooded by Hurricane Melissa in Santiago de Cuba, Oct. 29, 2025. (AP Photo/Ramón Espinosa, File)

Overview

  • Two peer-reviewed studies published June 10, 2026, analyze long tide-gauge records and climate models to separate human and natural drivers of sea level change and extreme coastal water levels.
  • The Climate Central-led paper finds a human signal at 97% of 519 tide gauges and attributes 58% of extreme-water days from 2000–2018 to sea level rise from human-caused warming.
  • A Tulane-led study shows events that had a 1% annual chance around 1900 are on average about 12 times more likely now and roughly four times more likely because of human-driven warming.
  • Local impacts are large and varied: Wellington’s 1-in-100-year coastal flood now occurs roughly twice a year in the study, and Galveston’s waterline has risen about 5.8 inches since 1900, with roughly 70% of high-water days in Southeast Texas linked to human causes.
  • Both teams note their results are conservative because some analyses end by 2005 or 2018, and they say findings directly affect infrastructure, insurance and planning by requiring updated flood-frequency estimates, stronger defenses, and clearer decisions on who pays for adaptation.