Let's define restoring force first: A force that tends to restore a disturbed ocean surface to a flat configuration (Intro. to Ocean Science, Douglas Segar).
So a restoring force works against a wave. Those forces are gravity, surface tension, and the Coriolis effect. Gravity is the primary restoring force for most waves. Surface tension tends to acts more prevalently on capillary waves (tiny wave heights). The Coriolis effect, which is not actually a "force," is the main restoring force for waves with long periods such as tides.
The restoring force in ocean waves is gravity, which pulls the water back towards its undisturbed position after a wave crest has passed. In the case of water ripples, surface tension acts as the restoring force, pulling the water molecules back into place.
The moving water particles return to their starting position due to the restoring force provided by surface tension and gravity. The energy from the wave causes the particles to oscillate but the restoring force brings them back to equilibrium position.
Gravity is the force of nature that pulls in Earth's water, keeping it on the surface of the planet. This gravitational force is responsible for the tides and the shape of the ocean basins.
An ocean vessel has a larger surface area compared to its weight, allowing it to displace enough water to generate buoyant force and float. In contrast, a nail has a smaller surface area relative to its weight, causing it to sink in water due to insufficient buoyant force.
An upwelling is a current in the ocean that brings deep, cold water to the ocean surface.
This section of the ocean from floor to surface is called the water column.
As long as any part of the object ... doesn't matter how much ... is below the surface of the water ... doesn't matter how far ... there is buoyant force on it.
As long as any part of the object ... doesn't matter how much ... is below the surface of the water ... doesn't matter how far ... there is buoyant force on it.
Conveyor Belt Cycling describes the movement of the ocean water between surface and deep water.
Stream like movements of water that occur near the surface of the ocean are called surface currents. Stream like movements of ocean water far below the surface are known as a deep current.
Evaporation occur at the surface of the ocean.
Surface Currents.