Sea Level Rise

The best I can do to summarise the complex subject of secular Sea Level Rise (SLR) is to start with Wikipedia:

“eustatic sea level has fluctuated significantly over the earth’s history. The main factors affecting sea level are the amount and volume of available water and the shape and volume of the ocean basins. The primary influences on water volume are the temperature of the seawater, which affects density, and the amounts of water retained in other reservoirs like rivers, aquifers, lakes, glaciers, polar ice caps and sea ice. Over geological timescales, changes in the shape of the oceanic basins and in land/sea distribution affect sea level. In addition to eustatic changes, local changes in sea level are caused by tectonic uplift and subsidence.” It is obviously difficult to differentiate eustatic SLR from crustal movements of the earth as our measuring instruments are placed on the earth. The best approach is to assess that water is supposed to remain ‘horizontal’ on a large basin like the Mediterranean Sea, while crustal movements occur at a more local scale (e.g. Crete). Hence, the average of all measured sea level movements on the entire basin will reflect the eustatic SLR, while local deviations from this average will reflect the local crust movements.

Sea Level Rise over the past 20 000 years (Wikipedia)
Sea Level Rise over the past 20 000 years (Wikipedia)
Sea Level Rise over the past 7 000 years (Wikipedia)
Sea Level Rise over the past 7 000 years (Wikipedia)

Many studies were conducted in recent decades to evaluate past SLR and to predict future SLR for the next century(s). The best known is the work of Kevin Fleming (1998)[3]. To make it short, the results are as follows, in round figures:

  • Predicted for the 21st c.: around 5 to 10 mm/year, and more
    depending on model used;
  • Observed in the 20th c.: around 2 mm/year;
  • Observed in the past 2000 years: around 0.25 mm/year,
    resulting in ca. 0.50 m SLR over this period;
  • Observed between 5000 BC and 0 BC: around 0.7 mm/year,
    resulting in ca. 3.50 m SLR over this period;
  • Observed between 13000 BC and 5000 BC: around 14 mm/year,
    resulting in ca. 110 m SLR over this period.

These figures are in accordance with work of Nic Flemming (1986)[1] who was the forerunner on this subject and with Christophe Morhange (2014)[2].

Since the rise of human civilisations around 5000 BC, SLR has been around 4 m. This value must obviously be combined with local crustal movements which may have reached several meters uplift (e.g. Phalasarna) or subsidence (e.g. Alexandria, Apollonia Cyrenaica, Portus Iulius, and many others).


[1] Flemming, N.C., Webb, C.O., 1986. “Tectonic and eustatic coastal changes during the last 10,000 years derived from archaeological data”, Z. Geomorphol. Suppl. 62, 1–29.

[2] Morhange, C., 2014, “Ports antiques et variations relatives du niveau marin”, Géochronique n°130, pp 21-24.

[3] Fleming, K., et al., 1998, “Refining the eustatic sea-level curve since the Last Glacial Maximum using far- and intermediate-field sites”, Earth and Planetary Science Letters 163, pp 327–342.