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Coastal Cities Face Accelerated Flood Risk as Land Sinks Faster Than Seas Rise

New research shows that in many densely populated coastal areas the ground is sinking at rates that make local sea-level rise three times the global average.

Scientists from the German Geodetic Research Institute at the Technical University of Munich and Tuline University have quantified how land subsidence amplifies sea-level rise for over half a billion people living in low-lying coastal zones. Their analysis, published in Nature Communications, reports an average relative rise of roughly 6 mm per year in densely populated coasts, nearly three times the worldwide coastline average and almost double the climate-driven absolute rise.

Major contributors include intensive groundwater pumping, oil and gas extraction, deltaic sediment compression and the sheer mass of urban development, alongside natural tectonic adjustments. Cities like Jakarta (13.7 mm/yr), Tianjin (13.5 mm/yr) and Bangkok (8.5 mm/yr) are identified as subsidence hotspots, with localized rates in Jakarta reaching 42 mm per year. Conversely, parts of Scandinavia experience uplift that offsets sea-level rise. The study highlights that policy actions—such as stricter groundwater regulation—have successfully reduced subsidence in places like Tokyo and the Harris-Galveston Subsidence District in Texas, suggesting a viable mitigation path for other vulnerable metropolises.

Why it matters

Accelerated land sinking intensifies flood threats for millions, demanding urgent urban and water-management policies.

In this story

coastal subsidencerelative sea-level risegroundwater extractionurban development weightclimate change impactflood riskmitigation policiesland sinking