California’s Big Kahuna

by on December 18, 2009

 

Peter Mel surfs a monster wave at Mavericks.

Public domain image from WikiMedia Commons.

 

 

From the shoreline, you can see bright dots of red, orange, yellow, green, and blue floating on the water’s crest. The colored dots are attached to men in black wetsuits. The two dozen invitees to this year’s Mavericks Surf Contest gathered on a sunny Friday at Pillar Point in Half Moon Bay to launch the opening of the 2009/2010 Contest.

This year’s waiting period lasts from November 1, 2009, to March 31, 2010, California’s big wave season. When the conditions are ripe, the 24 contestants vote to make the challenge a “go.” But they will ride no wave before it’s time. The biggest waves surfed are said to be as high as 70 feet, the height of a 4-story building. So what does it take to create these monster waves?

It alls starts in what’s known as the “wave factory” in the Gulf of Alaska, where storms gather thousands of miles away. This area experiences heavy activity from October to February when low pressure from the south clashes with high pressure in the north. Forecasters say that this year’s El Nino season will create a greater number of storms and thus larger surf than in previous years.

These faraway storms create three key ingredients that make winter our big wave season: wind velocity (how fast it’s blowing), “fetch” (how much surface water area that the wind is blowing over), and duration (how long the wind is blowing over that area). The recipe for big waves is a high dose of all three.

Tides and water depth also affect waves. When the tide is high, the water is deeper. When the tide is low, the water is shallower. As the tide moves from high to low, the wave energy goes to the sea floor, slowing down the wave but concentrating the energy upwards, intensifying the wave height.

But why doesn’t the whole coastline get big waves when the conditions are right?

The final ingredient is underwater topography. Without mountainous regions that rise steeply from the ocean floor, waves can’t become the monster waves at a place like Mavericks. As waves cross what surfers call a “launching pad,” the part of the wave that hits first will slow down, then bend into “V” formation, focusing the wave energy into one intense spot. This is called refraction. At this point, the energy explodes and wave height can more than double in an instant. The explosion is so intense at Mavericks that it registers on a seismograph.

To be part of this seismic action, check www.maverickssurf.com for the “go” sign and head to Half Moon Bay. Remember to bring binoculars as the waves break about a half mile out. If you want a view close up without the drive, the contest will be Webcast on internet and live by video feed at AT&T Park.

Another area known for monster waves is Ghost Tree, off the coast of the 18th hole of the Pebble Beach Golf Course in Monterey. Though it doesn’t break as often as Mavericks, it’s easier to see from land.

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2 comments:

Mavericks: The Science Behind the Killer Surf « Bay Nature on January 23rd, 2014 at 12:36 pm

[…] a quick explanation from a 2009┬áBay Nature story by Kris […]

Mavericks Competition: Why Surf Spot Has Monster Waves | RocketNews on January 25th, 2014 at 3:03 am

[…] reaches the seafloor. This energy has nowhere to go but up, increasing the wave’s height, according to Bay Nature, a San Francisco-area […]

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