Temporary flood risk from storm surges, permanent flooding from global sea level rise
e.g. Bangladesh and Tuvalu
Subsistance:
Low lying coastlines in estauries, deltas or outbuilding zones are subject to natural subsidence through the settling and compaction of recently deposited sediment
Deltas experience periodic isostatic subsidence
vegetation removal:
salt marshes and mangrove forest, reduces flood risk
Vegetation stabilises existing sediment and traps new sediment, raising the height of the land above sea level
Vegetation absorbs wave energy, reducing wave impact and erosion