Litoralströmung

Litoralströmung refers to the ocean currents that flow parallel to the coastline. These currents are primarily driven by a combination of factors, including wind, tides, and differences in water density. When wind blows parallel to the shore, it exerts a force on the surface water, causing it to move in the same direction as the wind. This effect is known as wind-driven coastal current. Tidal currents, generated by the gravitational pull of the moon and sun, also contribute significantly to litoralströmung, especially in shallower coastal areas. Furthermore, variations in water temperature and salinity can lead to density differences, creating pressure gradients that drive these currents.

The direction and strength of litoralströmung can vary greatly depending on geographical location, season, and local conditions. They play a crucial role in shaping coastlines by transporting sediment, nutrients, and marine organisms. These currents are vital for coastal ecosystems, influencing the distribution of species and the productivity of marine environments. They also impact human activities such as shipping, fishing, and coastal development. Understanding litoralströmung is essential for effective coastal management and for predicting the behavior of pollutants and debris in coastal waters.