Tides are the longest of all waves, with a wavelength that can equal half of the Earth’s circumference. As surfers, we wake up every morning thinking about the tides and how they may affect the quality of the overall surf. (Will the tide be drained, shallow, causing surfable waves at our reef or beach break to be heaving fast down the line (rideable face of the wave), possibly throwing steep barrels? Or…will the tide be high, swampy, with too much water over the reef or sandbars so the waves barely break, making for a slow, mushy, frustrating surf session?) Tides are periodic, short-term changes in the height of the ocean surface at a particular place. The California coast has a mixed tidal pattern: often a higher high tide, followed by a lower low tide, followed by a lower high tide, followed by a higher low tide each lunar day. A lunar day is 24 hours and 50 mins (the amount of time it takes for the moon to be in the sky at the exact same position as it was the night before), which means that the high and low tides arrive 50 minutes later each day. The reason for this is that the moon is orbiting Earth in the same direction as Earth’s axial rotation (the Earth rotates eastward). In California, the zero tide level is the average level of the lower of the two daily low tides.
The main cause of the tides is the gravity of the moon and the sun acting on the ocean. The forces that actually generate the tides varies inversely with the cube of the distance from the Earth’s center to the center of the tide-generating object (the moon or the sun). Distance is the most important in this relationship. The sun is 27 million times more massive than the moon (so it has a much larger gravitational force) but it is 387 times farther away than the moon so the sun’s influence on the tides is only about half that of the moon’s.
The moon does not revolve around the center of the Earth. Instead, Earth and Moon together—the Earth-Moon system—rotate around a common center of mass (1023 miles) beneath the Earth’s surface. As it revolves around Earth, the moon (gravity) attracts the ocean creating a tidal-bulge. The motion of the Earth (inertia) creates a second tidal-bulge on Earth, opposite side of the moon. Tides occur as Earth rotates (at nearly 1000 miles per hour given no interference like land masses, deep water, etc.) beneath these bulges. The bulges are the crests of the planet-sized waves that cause high tides. Low tides correspond to the troughs of the tidal waves.
The Ocean responds simultaneously to inertia and the gravitational force of both the Sun and the Moon. If the earth, moon, and sun are all in a line the lunar and solar tides will combine resulting in higher high tides…and lower low tides—this is called Spring Tides. If the earth, moon, and the sun form a right angle, the solar tide will pull opposite and decrease the lunar tide—this is called Neap Tides. Neap Tides occur at two-week intervals, a week after the spring tide.
Everything mentioned above is known as the equilibrium theory of tides (developed by Isaac Newton) and is this surfer’s (and writer’s) method of approximately predicting the tides. There are at least 140 tide-generating/tide-altering forces and factors. Seven of the most important of those must be considered in order to mathematically predict tides. Or simply check your local tide calendar because it is the study of past records that allows tide tables to be projected into the future with an accuracy of about 1.2 inches for years in advance. Even still, tides are difficult to predict as other things like storm surges, tsunami, onshore or offshore winds can all affect tidal height or the arrival time of the tidal crest (the high tide wave spanning half the earth’s circumference).
Remember that tides are a kind of wave. The crests of these waves—tidal bulges—are separated by a distance of half of Earth’s circumference. In the equilibrium theory, the crests of these waves would always point toward (or away from) either the moon or the sun as Earth turned beneath them. The dynamic theory of tides takes into account the speed of the long-wavelength tide wave in water of varying depth and how the moving water (tide wave) reacts with coastlines around the world. Due to the Coriolis effect, the tide waves move counterclockwise in the Northern Hemisphere (as the high tide moves in then withdraws to low tide in a particular place), and clockwise in the Southern Hemisphere. This can drastically affect the tidal range (height difference between high-water and low-water level). In California, the tidal range is a little more than 7ft. In the Bay of Fundy in New Brunswick (Canada) the tidal range is nearly 50 feet, leaving once docked boats lying in the sand at low-tide. As water (tidal current) rushes in our harbors, bays, and surf breaks it can actually temporarily improve the condition of the surf giving the wave an extra push (this is called a flood current). Often at high tides or low tides, the currents go completely still—slack tides—as the tides change direction. As the water rushes away from our coasts/surf breaks it causes an ebb current, which can create choppy, nearly unsurfable waves—as the tidal currents rush back out to sea like a river ripping through the waves. These (planet sized) tide waves can create tidal bores at narrow river mouths and inlets. A steep wave is created as the tide crest moves upstream, and the narrow river mouth forces the wave to move at a speed that exceeds the theoretical shallow water speed for that depth. The forced wave breaks forming a spilling wave that bores upriver. The Silver Dragon, the name for the bore on China’s Qiantang River may be up to 26 feet high and travel 25 miles per hour.
Check out this amazing footage of tidal bore surfing in Indonesia. Watch how the tidal crest forces its way upriver uprooting trees (1:05 minute mark):
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Wow this fascinating stuff. Really interesting to read.
Our Ocean ???? is an awesome wonder filled with more curiosities than the cosmos.(sorry Neil Degrasse Tyson!)
I certainly agree and the concept of tides fascinates me so much as the ocean breathes itself on this earth and our bodies too have an ocean inside. I must be amazing to surf and just feel that connection. I miss the ocean so much I used to live close to it for a couple of years but now I am inland. Keep posting all this fascinating info. <3
Tides, very little happenstance alongside much precise, awe inspiring creation! If the vast knowledge behind the making of a tide doesn’t make a God/Creator believer, it should at least make a better, wiser surfer! Super cool and informative article! Btw, tidal bore surfing… wholly WOW!
Our Universe is such an amazing “accident”…or is it ????…
Tides fascinate me as does the moon, I live where two oceans meet, and therefore two tides meet. So enjoyed reading this.
Where is it that you live pvcann? South Africa ???????? , Cape Of Good Hope, where the Atlantic and Indian Oceans meet? Cape Horn, southern Chile ????????, where the Atlantic, Pacific and Soutnern Oceans collide? Gulf Of Alaska? ????
On the southern corner of Western Australia, at a place called Augusta
A must read for all surfers!
Thanks Jay ???????? An understanding of the tides can totally help you score better waves ????
As a French science journalist, I love it when science, nature and beautiful writing collide.
Great article, but one bone to pick. As I understand it, gravity diminshes with the square of the distance, not the cube.
This quote is taken from and links directly back to the National Oceanic Atmospheric Administration.
Reblogged this on From 1 Blogger 2 Another.
Definitely educational and enjoyable reading!
A wonderful and informed post. As the sea and oceans always played a big role in my life I so agree on the healing and calming
effect. Waves and tides I have watched with fascination and understood a fair bit. You go further with your more exact
knowledge. I do like the drawings you included.
Did you take any of the wonderful photos? If so, congratulations.
Also thank you for your visit to my blog today.
[…] is so important. Every surfer worth their salt will take a moment to observe the following: wind, tide, swell direction, where the waves are breaking, where other surfers are sitting in the lineup, […]
Good info. Another nice byproduct of low tides is tide pools. What many people do not realize is that low tide itself may not be low enough. At Cabrillo National Monument on Point Loma in San Diego, for instance, the low tide had to be .7 or lower for the tidepools to be visible. Try explaining that to someone who has never lived by the ocean…
What a stunning wealth of information! Thank you for following BrewnSpew.
You make this surprisingly accessible to a non-technical person–which is another way of saying, to me. Thanks.
Thanks Ellen! ???? That’s a really nice compliment! I try my best to make things fun and easy to read, which usually requires a lot of work!
I share that goal with you. Simple’s a lot harder than complex.
Simple is so often harder than complicated.
How did I manage to say almost the same thing twice? Apologies. I don’t know much, but I do seem to say it often.
Wow…A wonderfully fascinating article, well written in layman’s language I could understand most of it…Thank you for choosing to follow my blog which led me in turn to this post.
Thanks, Carol. ???? I enjoy food almost as much as I enjoy surfing!
You have to keep your strength up as I am sure surfing requires lots of energy 🙂 Happy surfing 🙂
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