— Ch. 1 · Historical Observations And Trends —
Sea level rise.
~5 min read · Ch. 1 of 6
The global average sea level has risen about 20 centimeters since 1880. This steady climb accelerated dramatically after the 1970s, reaching a rate of 4.62 millimeters per year during the decade from 2013 to 2022. Paleoclimate data confirms this recent speed is faster than any time in at least the past three thousand years. A research paper published in October 2025 updated the global sea level curve for the last 11,700 years. It found that global mean sea-level rise since 1900 is faster than in any century over the last four thousand years. The longest running sea-level measurements began in Amsterdam in 1675 under the name NAP or Amsterdam Ordnance Datum. Data collection also started extensively in Australia with Thomas Lempriere establishing a benchmark on the Isle of the Dead near Port Arthur in 1841. These records combined with satellite data show the acceleration clearly. Between 1901 and 2018, the average sea level rose by roughly 20 centimeters. Satellite radar measurements from 1993 to 2017 showed an increase of 3.4 millimeters per year. This trend has continued to accelerate as human activities drive climate change.
Physical Drivers And Mechanisms
Three main forces push water levels higher today. Thermal expansion accounts for about 42 percent of the rise between 1993 and 2018. Melting ice sheets and glaciers contributed another 44 percent during that same period. Ocean heat content increased by 1.2 degrees Fahrenheit since 1950, contributing more than half of all observed sea level rise. When oceans gain heat, water expands and takes up more space. Warmer tropical water expands significantly more than cold Arctic water. Ice loss from Greenland added 10.8 millimeters to global sea levels between 1992 and 2018. West Antarctica lost mass at an accelerating rate after the year 2000. Thwaites Glacier now contributes 4 percent of total global sea level rise. Mountain glaciers contributed around 40 percent of historical sea level rise during the 20th century. Their contribution is expected to drop to roughly 30 percent in the 21st century but remains significant. Sea ice melting itself adds very little directly because floating ice displaces its own weight. However, land-based ice stores most of Earth's fresh water and drives the bulk of current changes.