Most of the buoys in the United States are run by the National Oceanic and Atmospheric Administration’s (NOAA) National Data Buoy Center. Individual buoys can be accessed on the internet via NOAA’s website. Here’s how to read them:
Wind, and more precisely, where it’s coming from and how fast, is the second most important surf-affecting variable other than wave size. It’s also constantly changing and difficult to predict with much precision. Because onshore wind (blows from the ocean towards land) is detrimental to surf conditions, and conversely, offshore wind (blows from land out to sea) is optimum, it’s a good idea to understand how to get up-to-date wind information from your local buoy.
The two variables that influence wind conditions are wind direction and wind speed, and both are important. Wind direction tells you the direction the wind is blowing from. Wind speed is the speed the wind is blowing, measured in knots. For example, if the buoy’s wind reading says the direction is NNW at 15 kts with 25 kts gusts, that means the wind is blowing out of the north/northwest, at 15 knots, with occasional gusts of up to 25 knots. For surfing, that’s a lot of wind, but if you have access to a break that faces south, the wind will funnel straight offshore.
This one takes the top honor in terms of importance to the surfer. If there are no waves, it really doesn’t matter what the wind direction is or how high the tide is – you’re not surfing anyway. And while all the surf-forecasting websites do a pretty decent job of giving you accurate swell information, any individual swell event goes through a lifespan that ranges from building, to peaking, to dying out, and eventually fading completely. Check in with your local buoy to see exactly what the swell is doing at that exact hour.
There are two variables that contribute to the size of a wave when it breaks: wave height and wave period. What? There’s more to waves than their height? Oh, you have so much to learn.
The period describes time elapsed between individual waves within a given wave set. For example, a period of 14 seconds means that when a set of waves reaches the beach, about 14 seconds will elapse in between each wave that breaks. Interestingly, a wave’s period is extremely significant because it directly affects both size and power. Period translates into the distance between two waves as well as the depth, meaning the longer, or deeper, a wave’s period, the bigger and more powerful it will be once it reaches its breaking point. Therefore, a wave with a long period will actually have more deep-water energy than a wave with a short period, giving it more height and power when it breaks.
A buoy’s wave height reading is exactly what it sounds like: the height, given in feet, from the peak of each wave to its trough. Keep in mind that buoys will automatically average out both the wave height and wave period.
So how do you determine actual wave height from both size and period? To know how a certain swell will affect your local surf conditions, you need to understand how particular breaks respond to both short period swell (also called wind swell) and long period swell. You also need to quantify the height and period into a single overall estimation of wave height. While experience is the only way to get really good at determining this somewhat elusive value, you’ll quickly learn that a swell reading six feet at 18 seconds is a lot bigger than one registering 10 feet at eight seconds.
In addition to wind and wave height, buoys also compute both air and water temperature.
Other Factors: Tide & Swell Direction
Tide and swell direction are secondary factors when determining surf quality, although both are extremely important. Blissful ignorance to tide and directions will only be blissful for so long.
Swell direction is an obvious factor when deciding when and where to surf. If a moderate-sized swell is rolling in from the south, you shouldn’t head to a beach that faces north unless you want to do more fishing than surfing. On larger swells, it’s sometimes wise to check spots that aren’t openly facing the brunt of the swell in order to access friendlier waves.
Ever wonder why surf shops give out those little tide books at the front counter? Every surfer should be aware of the day’s tidal scenario when deciding when and where to surf. Most surf spots have a particular tide that works best with that spot, and outgoing and incoming tides can affect rip currents and wave consistency. While some breaks may function on any tide, many more will altogether shut down if the tide is too low or too high. Getting to know your local surf spots and what tides they prefer is an important step towards getting quality surf as often as possible.
http://johnbarrett.net/wp-content/uploads/2020/11/L4_Buoy_RS_2.jpg6001500johnbarretthttp://johnbarrett.net/wp-content/uploads/2014/08/logo_flat_portfolio.pngjohnbarrett2020-11-03 19:40:162020-11-03 19:40:16How To Read The Buoys
Surfing is a cool way to spend a hot day—but there’s much more to riding waves than just balancing on a surfboard. Mastering surfing is all about mastering science: you need to know how waves travel across the ocean carrying energy as they go, and how you can capture some of this energy to move yourself along. Whether you’re surfing or bodyboarding, riding a longboard, or whizzing on a skimboard, you’re using cool science in a very cool way. Let’s take a closer look!
What are waves?
Waves are always the first thing you notice about the ocean. Except on very calm days, there are always waves skimming across the surface of the sea. What exactly are they doing there? We usually find waves in a place where energy has appeared. A basic law of physics called the conversation of energy says that energy can’t be created or destroyed; it can only ever be converted into other forms. When energy suddenly appears, concentrated in one place, something has to happen to it. Usually, energy doesn’t stay put: it tends to travel out in all directions to other places that don’t have as much.
The great thing about ocean waves is that you can see them coming. If you’re surfing, even fast-moving waves are slow enough to catch and carry you along. The properties of an ocean wave are also very easy to see. You can estimate its amplitude (height) just by looking out to the horizon. Its wavelength (the distance from one wave crest to the next) and frequency (the number of waves that travel past in a certain amount of time) are also very easy to see.
Where do ocean waves come from? If you live in the northern hemisphere, far from the equator, you’ve probably noticed that there are more waves around in the fall (autumn) or spring than in the summer. The wind is important because it’s what puts energy into the ocean: it makes ocean waves in more or less exactly the same way as you make sound waves when you bang the skin of a drum.
What’s the difference between wind swell and groundswell?
The waves that arrive at your beach are not necessarily created anywhere nearby. Back in the 1950s, an ocean scientist named Walter Munk conducted an amazing series of experiments with ocean waves. He managed to prove that some waves travel over 9000 miles across the open ocean before they reach their eventual destination. Generally, the more widely spaced and the cleaner waves are when they roll up on the shore, the further they have traveled.
Waves like this are known as swell (or groundswell) and they make the best waves for surfing. Groundswell is the reason you can have quite large waves washing up on your beach even when there’s little or no wind blowing. Waves generated nearby (by winds blowing in the local area) are known as wind swell. They are usually choppier, smaller, messier, harder to surf, and less interesting to surfers than groundswell. Often the waves in a particular place are a mixture of groundswell and wind swell—a random collection of waves that have traveled from far away mixed with waves that have come a much shorter distance.
Why is groundswell cleaner than windswell? When the wind blows on the sea, it produces all kinds of waves of different wavelengths, frequencies, and speeds. As the waves travel, the faster waves gradually separate out from the slower waves. The further the waves go, the more chance they have to sort themselves into an orderly pattern. Groundswell has more time to get itself into shape than windswell. Eventually, the waves form into distinct little groups called sets: when they finally arrive at their destination, a little group of good waves will arrive at once. Then there will be a pause. Then the next group of waves will arrive a bit later.
When and why do waves break?
Swell is only one of the ingredients for great surfing. Surfers don’t like any old waves: they want waves that peel (break gradually to the left or right along the wave crest) rather than close out (where the crest folds over and smashes to pieces all in one go). When a wave is peeling, you can ride back and forth across the crest as it slowly breaks; with a wave that’s closing out, there’s nowhere much to go. In surfing slang, waves that close to the right are called, not surprisingly, “righthanders”, while left-breaking waves are “lefthanders”. The angle at which the wave peels makes it more or less interesting to surf. The steeper the angle, the harder it is to surf and the more interesting moves you can pull.
What makes a wave break… and peel rather than closing out? When water flows, in the ocean, its upper layers are traveling faster than its lower layers. Think about waves arriving at a beach. As they travel from the open ocean to the shore, they move up a gradual sandy incline and start to slow down. The bottom of a wave slows more quickly than the top. So instead of a wave moving forwards as one, we have a whole series of water layers sliding past one another, with the top layers moving fastest and the bottom moving slowest. A wave breaks when the top part of the wave goes so far over the bottom part that the wave can no longer support itself—so it completely collapses. A wave peels when this process happens gradually along the length of the wave rather than all at once. If you like, a peeling wave is breaking in two dimensions: along the crest of the wave as the wave advances up the beach or reef.
Waves can break in many different ways, and that largely depends on the profile of the seabed underneath them (known as the bathymetry). All waves will break eventually, but major features like rock or coral reefs, ledges, and sandbars will make one side break before another, causing waves to peel. Nearby groins (sea fences), piers, and jetties can also make waves peel. Different shapes of reef produce different breaking effects.
Swell and bathymetry are not the only things that affect the quality of your surfing. How the wind is blowing on your beach will make a big difference too. Waves are obviously always traveling from the open ocean towards the beach, like scaled-up versions of ripples on a pond, but the wind can be blowing in any direction. If the wind is blowing directly out to sea, it is known as an offshore wind. As it blows, it will naturally tend to prop up the waves, stopping them from breaking so quickly, cleaning out some of the smaller choppier waves, and making the waves finally break with greater intensity in shallower water. A combination of strong ground swell and a light offshore wind is always best for surfing, especially if the wind has been blowing for a few days (both to create groundswell and to give it time to travel to your beach). If the wind blows in the opposite direction, so it is onshore, it will make the waves collapse much too soon—spoiling your fun! A strong wind that is blowing directly onshore (at right angles to the beach) can produce a very random, choppy sea that is impossible to surf, but fun to mess about in with a bodyboard.
Why do you have to paddle?
Science (and physics in particular) can explain most of the strange things you’ll notice when you’re riding along on your surfboard. Questions like why you have to paddle…
Whether you’re on a surfboard or a bodyboard, if a great wave is heading towards you, you have to paddle like mad to be able to catch it. In other words, you have to be traveling with some speed and momentum as the wave hits you to stand any chance of riding along with it. Why is that? To travel with a wave, you have to accelerate to the speed it’s traveling. In other words, you have to gain a certain amount of kinetic energy very quickly. If you’ve already got some kinetic energy to start with—if you’re already moving when the wave catches up with you—it’s much easier for the wave to accelerate you a little bit more. Or in simple terms, the faster you paddle, the more likely you are to catch your wave.
What about tides?
Tides have nothing to do with waves. Tides are caused by the Moon and the Sun working together to “pull” the sea back and forth with their gravity, rather like a giant blanket moving up and down a bed. Tides change the depth of the water on your beach. When the tide is “in”, the waves come in further and break later; when the tide is “out”, the waves break further out. Depending on the profile of the seabed, a rising tide (one coming in) or a falling tide (one going out) will make the waves tend to break somewhat better or somewhat worse than usual, depending on the local seabed. There is no absolute rule that works everywhere: some places work well as high tide approaches; some work best when the tide is going out.
When the Moon and Sun line up, twice a month, they make higher tides than usual called spring tides, which give deeper water during high tides (when the tide is in) and shallower water at low tide (when the tide is out). In between the spring tides are neap tides, when the sea moves back and forth less than usual, high tides are less deep, and low tides are less shallow. Again, depending on the seabed, high and low tides, and spring and neap tides, will make the surfing better or worse—but it varies wildly from place to place. If you’re in a place that needs deep water to make the waves break properly, the highest spring tides are going to be better than the lowest neap tides. But elsewhere, the opposite may be true.
Can science make you a better surfer?
Of course! It won’t make you stand on the board any better. But if you understand what waves are, how they are made, and where they come from, you’ll have a much better idea of when the surf’s going to be up. And if you can predict when the waves are ready to ride, you’re halfway there already. If surfing is a quest for the perfect wave, science can at least point you in the right direction.
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Blame the Sun. Blame the Sun for all your surfing-related problems—because that giant nuclear fireball, 150 million km (93 million miles) away, is surely to blame.
Like almost everything else on Earth, surfing is solar-powered: the energy that shoots you over the sea comes indirectly from the Sun. And what a lot of energy beams our way: theoretically, up to 1000 watts of solar power per square feet of land. But the interesting thing is not where this energy comes from, but where it goes. Earth’s lopsided tilt means the planet cooks unevenly in sunlight, like a spit-roasting joint we’ve stupidly propped at the wrong angle. The tropical bits can blacken and char to the point of forest fires while the polar caps (for now, at least) stay locked in ice. Because energy likes to even itself out, Earth has a turbulent atmosphere and an equally dynamic ocean. And where the howling winds meet the tumbling water, we get waves. Lots of waves.
What are waves anyway?
You know the answer to this question both in theory and in practice. In theory, because you can still remember flipping through the pages of your old school textbook: amplitude, wavelength, and frequency—those are officially the measure of waves. Now you’re older and a surfer, and you spend a significant part of your life bouncing up and down the sea surface, waves mean something different: breaking waves make your day. They’re no longer two-dimensional scientific abstractions—wiggly black lines drawn on white paper—but colourful, three-dimensional memories, vividly tied to places and times, burned in your memory till the day you die. Every science book explains waves the same way: as energy in motion, shooting from place to place while the medium (water, air, or whatever it might be) goes nowhere. But every surfer—even every beach-bound wave watcher—knows better than to reduce practical waves to a simple theory. Because, in glorious surfing reality, every wave is slightly different from every other wave that has ever broken in exactly the same place.
The waves surfers care about happen at the interface between the atmosphere and oceans, although they’re not the only waves you’ll find in either the air or the water. High above your head, there are waves shooting through the sky; that’s one of the reasons you’ll sometimes see cool, repetitive patterns formed in clouds (instead of the random lumpy cotton-wool you might be used to). There are also waves that travel deep underwater, but—intriguingly—often visible from high up in space.
How do waves form?
We all know the simple answer is “when the wind blows across the sea”, so the energy that was in the air is systematically transferred to the water. But how does that transfer take place? Is it like stirring a cup of coffee, except with friction from the wind dragging the water surface and tugging it along? It’s not hard to think of all kinds of ways the wind might stir up the water—but what does the science say?
Imagine the surface of the ocean is flat and glassy with not a wave in sight. Peer close enough and the water-air interface you see is no different from the mirror surface of a pond, where cunning insects float and scamper on invisible skin. Water has surface tension, just like a drum, and if you deform it slightly, the pulling force between neighboring water molecules will spring it rapidly back again. This is the first key bit of science in a glorious sequence of events that build the waves for surfing. Because as the wind starts to blow over water, it creates minuscule ripples called capillary waves, barely a foot high. The water’s own elasticity—surface tension—tries to destroy them immediately by tugging them back into place.
But with a steady wind blowing, it’s already too late: the water surface is roughening up. Now friction kicks in and the wind can get more of a grip, systematically building up the ripples to make wind chop and swell that will eventually clean itself up into perfectly formed surf in a voyage that could last hundreds or thousands of miles. Once waves grow beyond capillary size, surface tension can’t stop them. Now they’re at the mercy of the most persuasive long-range force in the Universe: gravity. Where surface tension does its best to rid the ocean of puny capillary waves, gravity is responsible for wrecking every surfer’s fun by cleaning away the bigger waves: it’s the force that determines the life and death of every ocean wave as it constantly tries to smooth out the sea.
A swell party
If you’ve ever played at making surf in your bored, Sunday afternoon bath-tub, by flipping your hand back and forth in the water, you’ll have figured out that there are three ways to make bigger waves: you can flip your hand faster, further, or for longer. The wind in a storm zone works exactly the same way when it’s making waves. If it blows faster, longer, or over a greater distance (technically called the fetch), it creates bigger waves. Why? Because bigger waves need more energy to create them (you have to lift more water up against the force of gravity, for one thing) and a faster wind blowing for longer, or over a bigger area of sea, is the way to get that energy into the water. That’s one key reason why open coastlines are so much better for surfing. The simple rule is that it takes energy, time, and distance to make great surf. The 20ft waves that delighted southern California surfers in August 2014, courtesy of Hurricane Marie, had had 800 miles to get their act together.
That begs another interesting question: just how big can waves ever be? If a hurricane blew for weeks or months over a long enough fetch of open water, would we get ridiculously big waves? “Yes” is the simple answer, but there’s still a scientific limit to how much waves can grow. Like houses of cards, waves are unstable structures that gravity is determined to collapse, sooner or later—with the added complication that they’re moving in the turbulent interface between the atmosphere and the ocean. Seven decades of oceanographic research has determined that waves don’t build beyond a certain steepness: the ratio of their length (measured between one wave crest and the one following behind) to their height (measured from crest to trough, or maximum to minimum) can never be more than seven to one. Waves break on the shore when the rising slope of the beach (or reef) increases their steepness beyond that critical ratio; out in the open ocean, the same limit applies, and we get white caps forming as gravity forces excessively steep waves into premature collapse.
In practice, when the wind blows across the water in a perfect-surf-creating storm, we reach an equilibrium. The wind keeps on adding more energy to the water, but the waves keep collapsing. At this point, we have what the oceanographers call a fully developed sea. The waves are as big as they’re ever going to get. All they have to do now is get themselves to the shore, where the surfers are waiting.
The birth of surf science
Surfing is essentially a 20th-century invention, and so is surf science. But who first had the idea to turn the wonder of waves into a scribble of mathematics —and why?
Surf science owes its birth to military manoeuvres. The pioneers of surf forecasting, Norwegian oceanographer Harald Sverdrup (head of the famous Scripps Institution) and his young American student Walter Munk, figured out how to predict wave heights from the wind speed, fetch, and duration while working for the US military during World War II. Fortunately, they also had loads of data to test their theory and quickly honed their equations enough to make accurate predictions. Although no-one knew it at the time, this crucial work was used by the Allied forces to select the best days for the famous beach landings. It was first used to pick a calm day for an assault on North Africa on 8 November 1942 and, subsequently, for the D-Day landings in Europe in June 1944. Surfing science, in other words, changed history.
Sverdrup and Munk completed their work in 1943, but it remained classified until after the War, finally appearing in March 1947 as US Navy Hydrographic Office Publication Number 601, “Wind, Sea, and Swell: Theory of Relations for Forecasting”. Later refined and extended by Charles Bretschneider, the revised theory became known as the SMB (Sverdrup, Munk, Bretschneider) model. Though it’s only a basic explanation of how the wind makes waves, it’s still widely referred to today, but it’s now been superseded by decades of more detailed research.
How much energy is there in waves?
It’s worth quantifying the energy in waves for all kinds of practical reasons. From an environmental point of view, it tells us how feasible it is to build things like renewable wave-energy systems—and whether we can harvest more energy from the hidden heat in ocean water (the temperature difference between the ocean surface and its depths) than from its mechanical energy (the back-and-forth, up-and-down movement of water caused by tides and waves). From a surfing point of view, asking this question tells us exactly which waves are rideable and what you can do on them. Everyone knows you can’t catch a small wave on a surfboard (or even a boogie board)—and the simple scientific reason for that is that a rideable wave needs to contain a minimum amount of energy to lift your body against the force of gravity and accelerate you to its own speed.
Let’s try to guesstimate how much energy there is in a medium-sized wave crashing down on top of us as we stand in the surf. I must emphasize that this is “back-of-the-envelope” physics and not in any sense rigorous or correct oceanography. It’s what’s technically referred to as “just a bit of fun”! I’m not going to attempt to use the complex equations that are really needed to do this properly. For now, let’s see how far we can get with the kind of basic science we learn at school.
We know the total energy is the sum of the wave’s kinetic energy (because the water is moving) and potential energy (because the crest is lifted up above the mean water level). Let’s not get too bogged down, though: let’s simplify everything as much as we can to the point of basic, school-level physics.
Suppose we have a 1m width of a wave that closes out completely, with the water coming to an impossible, screeching halt (so effectively it loses all its kinetic and potential energy when it breaks). According to Willard Bascom (one of the founding fathers of surf science), the speed of a decent surfing wave is about 25mph or 11 m/s. For easy sums, let’s assume the wavelength (the distance between one wave peak and the next one) is 2m and the amplitude (the height of the wave) is also 2m, so the volume of water above the mean sea level that we’re interested in (the dark grey bit in the figure is roughly 1 x 1 x 0.6 = 0.6m3 = 600 liters, which weighs about 600kg. Simplifying very greatly indeed (I know, I know… but bear with me), that gives us potential energy of mgh = 600 x 10 x 1 = 6000 joules and kinetic energy of ½mv2 = 300 x 11 x 11 = 37,000 joules, making a grand total of about 43,000 joules—or call it 50 kilojoules to keep things simple. This is a rough estimate of how much useful (non-heat) energy there is per foot of a simple breaking wave—and the actual value is likely to be less than this because of all the simplifications I made (a real wave isn’t this steep; it doesn’t stop completely when it breaks; it has an ever-changing, irregular volume; its total mass is not all concentrated at exactly the same height, and so on).
Do the numbers tell us anything useful? Suppose you weigh 70kg (not including the weight of your board). If you want to travel at 11m/s, you need kinetic energy of ½mv2 = 35 x 11 x 11 = 4235 joules. To ride a meter above the ocean surface, you’ll also need potential energy of mgh = 70 x 10 x 1 = 700 joules, so you’ll need about 5000 joules of energy altogether. Let’s say it takes you 5 seconds to catch the wave. The power your muscles and the wave need to supply for you to start surfing is the total energy needed to be divided by the time it takes, so that makes an average power of about 1000 watts to reach 5000 joules in 5 seconds—as much as a typical clothes washing machine. Could you get that from a 1ft wave? Maybe yes, maybe no. My estimate of about 50 kilojoules was for the total energy in 1ft width of a wave, which sounds like it’s 10 times more than enough—but, remember, you wouldn’t get all that energy from the wave (it keeps moving and doesn’t break) and you’re not tapping into a 1ft width of water (maybe only the width of your board).
Kids, lucky things, can catch smaller waves than adults because they weigh about half as much and they can accelerate faster. The potential and kinetic energy of a surfer are both linearly related to body mass, so if you have less mass, you need correspondingly less energy—making it more likely the wave will sweep you along. By the same token, if a wave is big enough, you can (theoretically) surf it in or on whatever you like.
How exactly does paddling help? If you’re paddling as you catch a wave, you’ve already given your body a certain amount of kinetic energy and momentum, so any oncoming wave has to provide you with less of the total energy you need to get moving: paddling, put very simply, gives you a head-start in terms of kinetic energy and momentum. It doesn’t help you with potential energy: unless you’re lying prone on a bodyboard, you’ve still got to get upright!
But different waves deliver very different force even if they contain the same amount of energy. Why? Waves that break faster produce more force, which is why a plunging wave that closes out in a shore-dump is more dangerous than a wave that peels gradually across its width. Simple physics tells us why: if two waves contain exactly the same amount of energy but one breaks five times faster than the other, it can (theoretically) deliver five times the force (because F=mv/t and if t is five times smaller, f is five times greater).
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