How much the sea has risen

Global ocean, 1808 to 2024

Global mean sea level and the extra volume of sea water it represents, in mm and cubic kilometres relative to the 1900-1909 average. These records are corrected for land movement, so they measure the ocean itself.

Sources:

Volume is the rise times the ocean surface area of 361.8 million km², so 1 mm is about 362 km³. The satellite series has 0.3 mm/yr added for the ocean floor still sinking after the ice age, which makes the basins hold more water without the surface showing it; that is the standard correction for turning surface height into volume. The Jevrejeva and satellite series are shifted to match Frederikse over the years they overlap. Lough Neagh holds about 3.5 km³.

The coloured bands stack up the causes. Warmer water expanding adds volume without adding water; everything else is water that was on land and is now in the sea. The causes add up to a little less than the observed rise, which is the unexplained part of the budget in the paper.

Around Ireland, 1918 to 2024

Annual mean sea level from every PSMSL tide gauge on the island, in mm relative to the Dublin 1960-1990 mean. These gauges measure the sea against the land they stand on.

Data: PSMSL Revised Local Reference annual means. Each gauge has its own datum, so each one is offset to match the gauges it overlaps with (median difference over shared years, using unflagged readings only). Belfast and Malin Head are tied to Dublin over 1938-1997. Portrush is tied to Dublin and Malin Head over 1996-2001, which is the weakest link in the chain (about 11 mm of uncertainty, from 6 shared years). The Marine Institute gauges that start in 2008 or later are tied to Portrush and Bangor, and Howth to those.

Corrections to the raw PSMSL records:

Trend of the combined record: about 0.1 mm/yr for 1918-1990, 2.3 mm/yr for 1990-2024. Castletownbere rises faster than its neighbours through 2008-2024, which may be local land subsidence or gauge drift; it is kept in. Much of the north of Ireland is still rising slowly after the last ice age, so these gauges understate the rise of the sea itself.

The time axis is logarithmic in years before a reference year; the slider moves that reference year, so older years get squeezed harder the further right it sits. Click a gauge to hide or show it. The running mean only uses visible gauges.