Under the waves

How SurfCheck works

A surf forecast tells you what the swell is doing out at sea. What happens next depends on the seabed under your break. SurfCheck gives you both: an hourly forecast for every spot, and the surveyed reefs, sandbars and channels that turn that swell into a wave.

240breaks with an hourly forecast
14breaks you can see in 3D
50breaks in the Wave Lab, each checked against the sea
0logins, paywalls or ads
Four layers

From the open ocean to your break

01

The forecast

Swell height, period and direction, wind and tide, every hour for every spot, with a score, and webcams where there are any.

02

The seabed

Depths from national seabed surveys, down to a few metres apart. Where nobody has surveyed, we fill the gap and show it grey.

03

The wave model

A wave model runs over that seabed in your browser. You watch swell slow, bend round the reef and break.

04

The check

We compare where the model breaks waves with satellite photos of where the sea actually broke.

Layer 02 · The seabed

See what's under the break

Ireland has mapped its seabed in more detail than most countries, through INFOMAR, the national programme run by Geological Survey Ireland and the Marine Institute. Survey ships and aircraft have measured the depth every few metres along much of the coast.

We've turned that survey into 3D scenes of Irish breaks, plus Supertubos in Portugal from its own coastal survey. The reef off Mullaghmore Head, the sandbars at Strandhill, and Tramore Bay, shallow for kilometres out, are all there to spin and zoom.

Then press Run swell. The waves you see are a model, drawn with their height stretched so you can see them, but the seabed is the survey, grey where we had to fill it in.

Deep water Shallow water Land Not surveyed

Open Seabed 3D · Flat maps of 49 breaks in the Seabed Atlas

Mullaghmore Head: 3 m swell at 14 s from the north-west. Big-wave reef, experts only. Run it yourself
Tramore: 1.8 m swell at 11 s from the south, slowing across a shallow bay. Run it yourself
Why breaks break where they do

The seabed is a lens

Swell can cross an ocean in a straight line, then change direction in the last few kilometres. The reason is depth. Once the water is shallow enough for a wave to feel the bottom, it slows down, and the shallower the water, the slower it goes.

A crest rarely meets shallow water all at once. The part over a reef or a point slows first while the rest keeps going, so the whole crest swings round towards the shallow ground. Energy gathers where the crests bend together and spreads out where they bend apart. The swell brings the energy; the seabed decides where it lands. That is why one point can be firing while the bay beside it is flat.

Two maps of Mullaghmore Head. White wave crests arrive straight from the north-west and curve round the head; amber lines show the paths the energy takes, bunching at the tip. The 16 second swell starts curving further offshore than the 8 second swell.
Mullaghmore Head on the measured seabed. White: wave crests, one wavelength apart. Amber: the path the energy takes; where amber lines bunch, waves are bigger. This picture uses the bending rule alone (Snell's law). Left (top on phones): 8 s swell. Right (bottom): 16 s. The full model in Seabed 3D adds spreading round corners, growth in shallow water and a breaking limit of 0.78 × depth.

Why long-period swell wraps further

A wave starts to feel the bottom at a depth of about half its length. An 8 second swell is about 100 m long, so it barely notices the bottom until the water is 50 m deep. A 16 second swell is about 400 m long and starts slowing in 200 m of water, often kilometres further out. It has more distance to bend, so it wraps further round points and into corners that short-period swell never reaches.

The rule only holds for one swell at a time. Real seas mix periods and directions, and currents bend waves too. Our model shares those limits; see what it can't tell you.

Speed of the crest, from linear wave theory. By 3 m deep every swell moves at nearly the same speed; what differs is how far out the slowing started.
Water depth8 s swell16 s swell
200 m12.5 m/s24.9 m/s
50 m12.4 m/s19.2 m/s
20 m11.1 m/s13.3 m/s
10 m8.9 m/s9.6 m/s
3 m5.3 m/s5.4 m/s
Layer 03 · The wave model

Change the swell and watch the break respond

The Wave Lab lets you set the conditions. Pick a break, then move swell height, period and direction, wind and tide. The sea redraws as you go.

Beside it, a plain readout: how big the waves get at the peak, whether they spill or plunge, whether the wind is cleaning them up, and an experimental "Will it barrel?" with its reasons.

Every break states how much of the seabed under it was measured and how much was filled in, graded A to C. Where the survey is too thin, the lab says "Not reliable here" rather than guess.

Open the Wave Lab

The Wave Lab at Strandhill: break picker by country, a seabed-in-3D card, and readouts for breaker height, breaker type, wind on the sea surface and the barrel reading.
The Wave Lab at Strandhill, Co. Sligo.
Layer 04 · The check

Checked against the real sea

A model that is never checked is a guess. So we checked ours against the only record we could find of where waves really break that covers every coast: satellite photos.

The European Sentinel-2 satellites photograph the coast every few days. On clear days since 2021, the whitewater shows exactly where the sea was breaking. For each photo we ran the model with that day's swell and tide and measured how far its surf zone sat from the real one.

30Close
11Fair
7Poor
2Too few photos

50 breaks, October 2026. Best on well-surveyed reefs and points, mostly within 20 m. Weakest in big Irish and Moroccan bays, where the survey stops short of the beach and the bay takes the edge off the swell. We publish the misses too.

Easkey, Co. Sligo, on six satellite passes: whitewater seen by the satellite in red, the model's breaking zone outlined in blue, with two charts comparing surf-zone size and breaking depth.
Easkey, Co. Sligo. Red is whitewater the satellite saw; the blue line is where the model breaks waves. Contains modified Copernicus Sentinel data.
Straight answers

What it can't tell you

Today's sandbars

Every survey is a snapshot from the year it was taken. Reefs barely change. Sandbars move with every winter's storms.

Currents and rips

The model has no currents, so it can't show rips, tidal races or wind against tide. Read the rip currents guide.

Sheltered bays

In deep bays the model is fed the open-ocean swell, so it breaks waves further out than the sea does. Lahinch, Inchydoney and Tramore say so on the page.

Who should paddle out

The model shows a wave's shape, not whether it's a good idea for you. That depends on you, the day and the people in the water.

Not a safety or navigation service. Check the forecast, watch the water before you go in, and never surf alone. In an emergency at sea in Ireland or the UK, call 112 or 999 and ask for the Coast Guard.

Surf safety · Rip currents · RNLI water safety · Water Safety Ireland

Seabed 3D

The seabed under every scene

Tap one to open it in 3D.

Questions

Common questions

Are Seabed 3D and the Wave Lab forecasts?

No. The spot pages carry the forecast: swell, wind and tide, every hour. Seabed 3D and the Wave Lab are teaching tools. They show how a seabed shapes swell. They don't know today's sandbars, currents or crowds, so never use them to decide whether to paddle out.

Where does the seabed data come from?

In Ireland, from INFOMAR, the national seabed mapping programme run by Geological Survey Ireland and the Marine Institute. Elsewhere from EMODnet, the Environment Agency and UK Hydrographic Office in England, NOAA in the US, New South Wales in Australia, and Portugal's coastal LiDAR survey. All open data, credited on every view.

How accurate is the wave model?

We check it against satellite photos of whitewater. At 50 breaks (October 2026), 30 matched closely, 11 fairly, 7 poorly and 2 had too few clear photos to judge. It is best on well-surveyed reefs and points and weakest in big bays where the survey stops short of the beach.

Are the sandbars up to date?

No. Every survey is a snapshot from the year it was flown or sailed. Reefs barely change. Sandbars move with every winter's storms, and beach breaks carry that warning.

Does SurfCheck cost anything?

No. SurfCheck is free, with no login, no paywall and no ads.