The force and speed of wind will determine how little and big the waves are.
using sonar waves
The size of waves is determined by factors such as wind speed, wind duration, and the fetch (the distance over which the wind blows). The longer and stronger the wind blows over a larger area of water, the bigger the waves will be.
2 factors determine the size of the waves:
the lenght of the waves , strenght of the waves and the duration o the high waves determine how high the waves in a place will be
Winds generate waves by transferring their energy to the water's surface. The strength, duration, and direction of the wind determine the size and shape of the waves. Waves can travel great distances from where they were generated, making wind a key factor in shaping oceanic conditions.
The three factors that determine the size of a wave are wind speed, wind duration, and the fetch (the distance over which the wind blows without obstruction). These factors collectively influence the energy transferred to the water surface, which in turn affects the size of the waves.
Echolocation uses sound waves to navigate and locate objects in its environment. These sound waves are produced by the animal or device using echolocation, and they bounce off objects, returning echoes that are then detected to determine the object's location, size, and shape.
A wave gauge or wave recorder is the tool used to determine pitch in waves. It measures the height and frequency of waves, which can then be used to calculate the pitch of the waves.
The size and shape of the Earth's core can be used to measure its properties by studying seismic waves that pass through the Earth. By analyzing how these waves travel and are affected by the core's size and shape, scientists can determine important properties such as density, composition, and temperature of the core.
Scientists use seismographs to measure the magnitude of earthquakes. Seismographs detect the seismic waves generated by an earthquake, and the amplitude of these waves is used to calculate the earthquake's size. The most common scale used to measure earthquake size is the Richter scale or the moment magnitude scale.
Waves are mechanical energy that has been transferred mostly from wind. The factors that determine the size of an ocean wave made by the wind are: time of contact, velocity of wind and the fetch-distance over which wind is in contact with water.
When waves strike a barrier with a gap, they diffract or spread out as they pass through the gap. This diffraction causes the waves to bend around the edges of the gap, creating a pattern of interference on the other side of the barrier. The size of the gap relative to the wavelength of the waves will determine the extent of diffraction.