Mostly by erosion but if it deposits briny water, that will also decrease fertility
low-lying coastal areas during hurricane (cyclone) season
The death of a midlatitude cyclone typically occurs when it moves into an area of unfavorable atmospheric conditions, such as stable air or a decrease in temperature gradients and moisture availability. This can cause the cyclone to weaken and eventually dissipate, bringing an end to its life cycle. Additionally, interaction with land or encountering upper-level winds can also contribute to the decay of a midlatitude cyclone.
no
RAF Coastal Area was created in 1919.
An area of low pressure formed, which made the cyclone.
The eye of the cyclone is the calm weather found at the centre of the cyclone. It is the only part of the cyclone where clear skies are visible. The eye can range from 10km in diameter to 100km in diameter.
The area of Exmoor Coastal Heaths is 17.583 square kilometers.
The eye of a tropical cyclone is an area of calm, usually clear weather at the center of rotation.
australia
The calm area of a tropical cyclone is the eye. The circular eye of the storm is surrounded by a high wall of thunderstorms where the most severe weather occurs.
The area of Savannah Coastal Refuges Complex is 226.624 square kilometers.
The area of California Coastal National Monument is 4,046,856.4224 square meters.