Waves are actually a concentrated form of solar energy.Uneven heating of the Earth’s surface causes wind, and waves are generated by wind blowing over a distance of water. That distance is referred to as the fetch. Still not making sense? Try this. The best way to understand waves as energy is to think of a long rope laid on the ground. If you pick up one end and give it a good snap — there’s a ripple effect all the way to the other end — just like the waves on the ocean! That means that energy is applied at one end and it moves to the other end. The energy is released at the other end of the rope, just as the energy of a wave is released on the beach.
A very hard wind blowing for a long time over a large expanse of ocean will lead to large, frothy white caps. These eventually become large waves, which is why surf conditions are often good after a storm at sea. Satellite data used to track surface winds from outer space has helped forecasters predict where the surf will be high based on oceanic weather patterns.
As these peaks move away from the wind, they spend some of their energy through motion. This causes the peaks to smooth out into rounded swells. The swells collide with one another, and some of them combine through constructive interference. The larger, rounded swells begin to travel in approximately the same direction as the prevailing wind that originally created the whitecaps.
The swells become breaking waves when they reach shallower water. This can happen at the shoreline, at a point extending into the ocean or when the waves pass over an obstruction like a sandbar or a reef. Here’s what happens when the wave gets to water that’s about half the depth of its wavelength: The swells slow down as the water beneath them gets shallower. As a result, the waves get closer together, much the way a line of cars will get closer together if the car in front starts to slow down.
The leading edge of the swell becomes increasingly vertical as it slows while the trailing edge continues to look like a rounded slope. The waves get taller as the solid surface under them and the waves’ energy pushes the water upwards. Eventually, the wave crests, or breaks — the fast-moving back of the wave spills over the slowing front of the wave. The exact shape of the ocean floor has a dramatic difference on how the waves break. If the shore slopes gently upward, the wave will gently spill over as it crests. A steep slope can cause waves that break suddenly and dramatically. The cresting waves can travel for thousands of miles before reaching shore and becoming conducive to surfing. They have an enormous amount of power and momentum. For these and other reasons, they can become dangerous to even experienced surfers.
Gabrielle has regenerated into a TS with winds of 40 mph. TS Warnings are in effect for Bermuda. The system will affect Bermuda during the next 24-36 hours.
TS Humberto is nearing hurricane intensity and should become a hurricane quick enough so that the record for the latest first hurricane in the Atlantic basin is not broken. The system will stay out in the open Atlantic.