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Depending on height at origin as it approaches the coastal shelf it will rise and increase the strength of the wave. for example a wave 50ft high approaching the atlantic coastal shelf could rise to 150-200 feet with disastrious ramifications.
they get shorter
Depending on height at origin as it approaches the coastal shelf it will rise and increase the strength of the wave. for example a wave 50ft high approaching the atlantic coastal shelf could rise to 150-200 feet with disastrious ramifications.
A wave's energy moves in a circular pattern and the deeper the water column, the faster the wave travels and the smaller its size e.g. it has low steepness. As it approaches the shore and the water becomes shallow, the bottom of the wave drags on the ocean floor which slows the bottom of the wave down but the top of the wave continues at the same speed. Eventually the top of the wave gets so far ahead of the bottom that it topples over forming a breaker.
Since we don't know what "this wave" is, we cannot answer the question.
The wave would slow down as it approaches the shore.
The wave would slow down as it approaches the shore.
Breakercrest
Ocean water within a wave moves in a circular motion in open water. As the wave approaches the shore, the water becomes shallow and the bottom.
Depending on height at origin as it approaches the coastal shelf it will rise and increase the strength of the wave. for example a wave 50ft high approaching the atlantic coastal shelf could rise to 150-200 feet with disastrious ramifications.
Friction with the sea bed/shore
It is aclled an high tide
Of course it can. That is why some waves don't reach the shore.
true
it keeps on slowing down and hitsthe shore.
It feels like its real but you know youre acting.
I believe that they are bottom feeders......