Elevation changes such as tidal fluctuations are significant determinants of coastal and estuarine flooding.

The tidal fluctuation noted every 6 hours is of the order of 1 ft at the harbor.

These tidal fluctuations result in dissipation at an average rate of about 3.7 TW.

Its sheltered harbor is protected from tidal fluctuations.

The tidal fluctuations can be observed well with the exposure of oyster beds and roots during low tide.

The tidal fluctuations are playing a major role in dispersing the mangrove seeds.

Characterized by tidal fluctuations, these rare and fragile ponds are home to unusual plants and animals.

Head of tide is the farthest point upstream where a river is affected by tidal fluctuations.

The sea approaches are protected by extreme tidal fluctuations and extensive mud flats.

The tidal fluctuations play a major role in dispersing mangrove seeds.