Outdoor Education…Character development through the outdoors
Everything on Earth is driven directly or indirectly by the Sun's energy. The uneven heating of the Earths surface by the sun is the first link in a chain of events leading to cyclones, thunder storms, blizzards and those ocean-borne depressions responsible for the waves a surfer rides.
Land and water respond differently when heated and cooled. While the temperature on continents swings many tens of degrees from winter to summer, the oceans keep a more constant average temperature. So summer means warm land, not-so-warm sea. And winter means cold land, not-so-cold sea. Therefore, in winter air movement is a lot more than in summer.
The main creator of waves is wind blowing over the surface of water. At first, ripples are formed on a calm surface, which are easier for wind to get a grip on and increase their size.
As ripples grow, small disturbances of rotating air form between the ripples adding more height to the waves, which in turn creates more uniform pockets of turbulence between the quickly growing waves. Surface tension is no longer strong enough to restore the rippling disturbance and gravity now attempts to push the waves back down.
This cycle increases wave height until gravity limits further growth and the wave reaches saturation point.
This weather map shows a strong south westerly flow over New Zealand. The orange arrow shows the direction of the wind and therefore swell. In this situation, Auckland’s West Coast beaches would be hit by a very large swell.
Waves will break when the bottom part of the wave is slowed down so much that the top of the wave overtakes it and spills forward.
A sea-breeze (or onshore breeze) is a wind from the sea that develops over land near coasts. It is formed when hot air rises off the land causing cooler sea air to fill the space left, creating a cooler breeze near the coast.
The strength of the sea breeze is directly proportional to the temperature difference between the land and the sea. Sea breezes usually occur in the afternoon.
An on-shore wind blows towards the coast, causes waves to crumble and increase in energy.
An off-shore wind blows from the coast, keeps a wave clean and reduces energy.