4. Sea level measurements from tide gauge records in geologically stable environments show a rise of around 20 cm per century (2 mm/year). (Douglas ,1997) Changes in sea level since the end of the last glacial episode
5. Melting Ice Thermal Expansion Coral Bleaching Coastal modification Coastal Erosion Beach Loss Turtle nesting Water aquifers Human Settlement Infrastructure Port facilities Tourism Soil Salinisation Agriculture Wetlands SEA LEVEL RISE Poor management Mangrooves Fisheries FreshWater