What causes the wave height of a tsunami to increase as it comes into a shore?
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What causes the wave height of a tsunami to increase as it comes into a shore?
In deep water, a tsunami moves very fast and has a long wavelength and a small amplitude. As it enters shallower water, it slows down and the wavelength decreases. This causes the wave to become much taller. Having a shorter wavelength means that the waves get higher.
Why does the wave height of a tsunami increase as the tsunami enters shallow water?
Why does the wave height of a tsunami increase as the tsunami enters shallow water? -In shallow water, the wind driving the tsunami must push a larger water column. -In shallow water, the energy of the tsunami must be contained within a larger water column.
What causes the height of a wave to increase?
Wave height is affected by wind speed, wind duration (or how long the wind blows), and fetch, which is the distance over water that the wind blows in a single direction. If wind speed is slow, only small waves result, regardless of wind duration or fetch.
What causes the height of a tsunami?
From the area where the tsunami originates, waves travel outward in all directions. Once the wave approaches the shore, it builds in height. The topography of the coastline and the ocean floor will influence the size of the wave. There may be more than one wave and the succeeding one may be larger than the one before.
What happens when tsunami enters shallow water?
As the tsunami hits shallower water, the velocity slows, wavelength decreases and the waves height (amplitude) increases. Tsunami waves can grow up to 30 meters in height as they hit the shoreline and are followed by more waves that may even be more dangerous.
What is the height of tsunami waves?
Tsunamis may reach a maximum vertical height onshore above sea level, called a runup height, of 98 ft. (30 meters). A notable exception is the landslide-generated tsunami in Lituya Bay, Alaska in 1958, which produced a 1722 ft. wave (525 m).
What is the wave height quizlet?
The horizontal distance between two successive troughs is called the wave height.
How is the height of wave determined?
Explanation: Wave height is determined by wind speed, the duration of time the wind has been blowing, fetch and by the depth and topography of the seafloor. A given wind speed has a matching practical limit over which time or distance will not produce larger waves.
What is wave height in geography?
A wave’s height is the vertical distance between a crest and a trough. The wavelength of a wave is the horizontal distance between two crests or troughs. For wind generated ocean waves, it can vary from a few tens of centimetres to hundreds of metres.
What happens to the wavelength and height of tsunami waves as they approach land from the open ocean?
As the waves approach the coast, their wavelength decreases and wave height increases. On the open ocean, the wavelength of a tsunami may be as much as two hundred kilometers, many times greater than the ocean depth, which is on the order of a few kilometers.
Why does wave speed increase with depth?
Wave height stores the energy as potential energy. As a wave enters deeper water the height and potential energy decrease. Therefore the speed of the wave must increase.