The wind transfering some energy to the water and forming waves. Hence when its windier, you get bigger waves
Surface waves are primarily caused by earthquakes rather than winds. Earthquakes generate seismic waves that propagate along Earth's surface, leading to ground shaking. Winds, on the other hand, primarily generate ocean surface waves rather than seismic surface waves.
The most familiar kind of surface wave is an ocean wave, which is caused by the wind transferring energy to the water's surface. These waves can vary greatly in size and strength, depending on factors such as wind speed and duration.
Most surface waves are caused by the wind blowing over the surface of the water, creating ripples and waves. Other factors that can cause surface waves include seismic activity, tides, and underwater landslides.
Usually waves in the ocean are caused by wind since out in the ocean there is nothing to block, or slow down the wind because there's obviously no buildings or people usually around so the wind can be stronger and faster creating waves in the water.
The immediate energy source for most waves on the ocean surface is wind. Wind transfers its kinetic energy to the ocean surface waters, causing them to generate waves through frictional interaction.
Surface waves are caused by the interaction between seismic waves and the Earth's surface. These waves travel along the Earth's crust and can cause the ground to shake horizontally and vertically. Surface waves are typically the most destructive type of seismic waves during an earthquake.
Seismic waves, specifically surface waves, can affect the surface of the land by causing it to rise and fall like waves on an ocean. These waves are typically generated during an earthquake and can produce the most visible effects on the Earth's surface.
Tsunamis are the most destructive waves in the ocean, typically caused by underwater earthquakes, volcanic eruptions, or landslides. Their long wavelengths and high speeds make them capable of causing widespread devastation when they reach coastlines.
The gravitational pull of the moon combined with the gravitational pull of the earth causes the water to be pulled back and forth.
Ocean waves are formed by the wind transferring its energy to the surface of the water. When the wind blows across the surface of the ocean, it creates ripples that then develop into waves. The size and power of the waves depend on factors such as wind speed, duration, and fetch (the distance over which the wind blows).
Most ocean waves obtain thier energy and motion from
No, P and S waves travel faster than surface waves. P waves are the fastest seismic waves, followed by S waves, with surface waves being the slowest. Surface waves are responsible for most of the damage caused by earthquakes due to their amplitude and duration.