New Study: Sea Levels Rose 20 Times the Modern Rate During the Roman Warm Period

A picturesque view of an ancient Roman-style city with grand architecture, large domes, and statues along a river. Several boats are docked, and people are gathered along the shore, showcasing vibrant sails and a lively atmosphere.

From No Trick Zone

By Kenneth Richard 

“[D]uring the last 6 ky, repeated, meter-scale, rapid (<300 y) rises alternated with meter-scale falls…interpreted as global.” – Higgs, 2026

new study uses excavation evidence (wall ruins, coins, pottery) to suggest sea level rise (SLR) rates reached ~4 m in ~70 yrs (60 mm/year, or 20 times the modern rate of 3 mm/year) from 430 to 500 CE across southern England.

Sea levels reached 3 m higher than today ~1500-2000 years ago, concurrent with the Roman Warm Period. Consequently, the coasts were 1.5 – 3 km farther inland versus today at this time.

Sea level falls were similarly rapid (for example, ~2 m in less than 100 years). Indeed, “dozens of authors found further evidence for Holocene SL [sea level] fluctuations of up to 5 m.”

These SLR rates were absolute or eustatic (due to water loading from melted ice sheets), and the fluctuations were likely global in scale. Similar meters-per-century SLR rates occurred in New Zealand, France, Brazil, and Florida (USA) during this period.

A research poster detailing the archaeological evidence of a four-meter sea-level rise in England during the fifth century, including graphs, maps, and analysis related to coastal changes and historical context.
Image Source: Higgs, 2026

2024 study indicated that, 8200 years ago, near-global sea levels rose 6.5 meters in a span of just 140 years. This is 470 centimeters per century, 4.7 centimeters per year, during a period when CO2 levels were alleged to be a “safe” and stagnant 260 ppm.

A scholarly article discussing Holocene human-environment interactions in southern Australia, focusing on the Ngurunderi narrative and sea-level changes over time. Includes a graph showing relative sea levels at various locations along the Australian coast over thousands of years.
Image Source: Nunn et al., 2024

The net melt of the Greenland ice sheet (GIS) is thought to have been the largest contributor to sea level rise in recent decades. But, to put the GIS change in context, the entire ice sheet melt contribution to sea level rise was just 1.2 total centimeters from 1992-2020 (Simonsen et al., 2021).

Satellite radar-altimetry mass balance of Greenland Ice Sheet (GrIS) showing changes in mass loss from 1992 to 2020. Panels (a) and (b) depict early satellite data with limited mass loss and accelerating mass loss respectively, while panel (c) illustrates significant mass loss in the Baffin area.
Image Source: Simonsen et al., 2021


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