Where do ocean waves come from? What gets them started? In
fluid dynamics, wind waves or, more precisely, wind-generated waves are surface
waves that occur on the free surface of oceans, seas, lakes, rivers, and canals
or even on small puddles and ponds. They usually result from the wind blowing
over a vast enough stretch of fluid surface. Waves in the oceans can travel
thousands of miles before reaching land. Wind waves range in size from small
ripples to huge waves over 30 meters high. When directly being generated
and affected by the local winds, a wind wave system is called a wind sea. After
the wind ceases to blow, wind waves are called swell. Or, more generally, a
swell consists of wind generated waves that are not—or hardly—affected by the
local wind at that time. They have been generated elsewhere, or some time
ago. Wind waves in the ocean are called ocean surface waves .
Motion of a particle
in a wind wave.
A = At deep water.
The orbital motion of fluid particles decreases rapidly with increasing depth
below the surface.
B = At shallow water
(sea floor is now at B). The elliptical movement of a fluid particle flattens
with decreasing depth.
1 = Propagation
direction.
2 = Wave crest.
3 = Wave trough.
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