Friday, September 27, 2013
THE Surf Report
Falling for fall.
SURF:
Man did fall kick in on schedule. NW windswell the past few days, cool temps, and breezy conditions. Heck, they even had snow in the Sierras. And as the weak cold fronts typically blow through in fall, we get high pressure behind them with varying degrees of offshore winds.
This morning we have dying NW windswell with a touch of tiny SW for shoulder high sets in SD and maybe an inconsistent chest high set in north county and the OC.
Look for great conditions this weekend as the NW dies off and the SW fills in slightly for waist high waves in north SD county and the OC. All in all nice weather this weekend and a little bit of surf.
Water temps are 67 and tides the next few days are really mellow- about 3' at sunrise and 4' at sunset. Make sure to keep up to date on the waves/weather at Twitter/North County Surf.
FORECAST:
After the little NW and SW and nice conditions this weekend, more NW swell moves in late Monday. That lasts into Wednesday morning.
We also had a good late season storm in the southern hemisphere yesterday (finally) and we have some SW swell headed our way for late Tuesday into Wednesday. Hopefully the weak cold front forecasted for mid-week (see below) won't be as strong as the models indicate so our surf will stay clean!
WEATHER:
Typical fall- a few days of clouds, breezy weather, and cool temps- then high pressure kicks in for warm weather, offshore winds in the AM, and not a cloud in the sky. Then of course the clouds will return, the wind will kick up, and everything just keeps rotating. That's what we have in store- the clouds/breeze yesterday has been replaced by high pressure and temps near 80 at the beaches later today and tomorrow. That will last into Sunday. Then another weak front moves down from northern California on Tuesday and we get clouds and breezy conditions mid-week. Models then show high pressure building towards next weekend and yes- more sunny skies and warm temps at the beaches.
BEST BET:
Looks like Tuesday with the peaking NW swell and building SW swell. Just keep your fingers crossed the next weak cold front from northern California is just that- weak.
NEWS OF THE WEEK:
There's been a few famous debates about big waves over the years, like how big was Greg Noll's wave at Makaha '69? What caused Mark Foo to drown at Mavericks? Did Garrett McNamara really ride a 100' wave in Portugal? Well now there's a new question to ponder: Scientists have discovered breaking deep sea waves, as high as 800' tall on the ocean bottom. Science Daily broke the story earlier this month:
Waves breaking over sandy beaches are captured in countless tourist photos. But enormous waves breaking deep in the ocean are seldom seen, although they play a crucial role in long-term climate cycles. A University of Washington study for the first time recorded such a wave breaking in a key bottleneck for circulation in the world's largest ocean. The study was published online this month in the journal Geophysical Research Letters. The deep ocean is thought of as dark, cold and still. While this is mostly true, huge waves form between layers of water of different density. These skyscraper-tall waves transport heat, energy, carbon and nutrients around the globe. Where and how they break is important for the planet's climate. "Climate models are really sensitive not only to how much turbulence there is in the deep ocean, but to where it is," said lead author Matthew Alford, an oceanographer in the UW Applied Physics Laboratory. He led the expedition to the Samoan Passage, a narrow channel in the South Pacific Ocean that funnels water flowing from Antarctica. "The primary importance of understanding deep-ocean turbulence is to get the climate models right on long timescales," Alford said. Dense water in Antarctica sinks to the deep Pacific, where it eventually surges through a 25-mile gap in the submarine landscape northeast of Samoa. "Basically the entire South Pacific flow is blocked by this huge submarine ridge," Alford said. "The amount of water that's trying to get northward through this gap is just tremendous -- 6 million cubic meters of water per second, or about 35 Amazon Rivers." In the 1990s a major expedition measured these currents through the Samoan Passage. The scientists inferred that a lot of mixing must also happen there, but couldn't measure it. In the summer of 2012 the UW team embarked on a seven-week cruise to track the 800-foot-high waves that form atop the flow, 3 miles below the ocean's surface. Their measurements show these giant waves do break, producing mixing 1,000 to 10,000 times that of the surrounding slow-moving water. "Oceanographers used to talk about the so-called 'dark mixing' problem, where they knew that there should be a certain amount of turbulence in the deep ocean, and yet every time they made a measurement they observed a tenth of that," Alford said. "We found there's loads and loads of turbulence in the Samoan Passage, and detailed measurements show it's due to breaking waves." It turns out layers of water flowing over two consecutive ridges form a lee wave, like those in air that passes over mountains. These waves become unstable and turbulent, and break. Thus the deepest water, the densest in the world, mixes with upper layers and disappears. This mixing helps explain why dense, cold water doesn't permanently pool at the bottom of the ocean and instead rises as part of a global conveyor-belt circulation pattern. The Samoan Passage is important because it mixes so much water, but similar processes happen in other places, Alford said. Better knowledge of deep-ocean mixing could help simulate global currents and place instruments to track any changes. On a lighter note: Could an intrepid surfer ride these killer deep-sea waves? "It would be really boring," admitted Alford, who is a surfer. "The waves can take an hour to break, and I think most surfers are not going to wait that long for one wave." In fact, even making the measurements was painstaking work. Instruments took 1.5 hours to lower to the seafloor, and the ship traveled at only a half knot, slower than a person walking, during the 30-hour casts. New technology let the scientists measure turbulence directly and make measurements from instruments lowered more than 3 miles off the side of the ship. The researchers left instruments recording long-term measurements. The team will do another 40-day cruise in January to collect those instruments and map currents flowing through various gaps in the intricate channel.
BEST OF THE BLOG:
Seen the new Arnette building in downtown Encinitas? What exactly is it? A retail store? Offices? Party headquarters? Yes, yes, and yes. Check out the full story on the blog. And of course a mid-week Surf Check and an in-depth THE Surf Report. All of that and more in the blog below!
PIC OF THE WEEK:
Secret spot #12873-C. I can sell you a map to this place. Gonna cost you though...
Keep Surfing,
Michael W. Glenn
Global Sensation
In A Wham! Cover Band
Patented The Surfboard