


Rising sea levels
Sea level rise is mainly due to two factors related to global warming: the additional water from melting ice sheets and glaciers and the expansion of sea water as a result of rising temperatures.
Observations show that since 1900 to the present day the level of the world oceans has risen by about 21 cm. According to scientists, in the last 30 years the rise of the sea level is due to:
- the expansion of water due to its warming – about 42%,
- melting of glaciers in temperate latitudes – 21%,
- melting of snow and glaciers in Greenland – 15%,
- melting of the ice cap of Antarctica – 8%.
In the 21st century, as a result of the continuing global warming the pace is expected to accelerate further. The latest measurements show that sea levels are currently rising by 3.6 mm per year.
Rising sea levels are crucial for coastal states. One third of the population the European Union lives within 50 km of the coast. The consequences of sea level rise include flooding and wetland displacement, coastal erosion, increased salinity and the need for drainage.
By 2100, sea levels are expected to rise by about 60 cm from early 21st century levels, and some more pessimistic forecasts suggest up to 90 cm. The Arctic region will be one of the worst affected. The Baltic, Mediterranean and Black Sea regions are also at risk.