This section covers everything you need to know about waves and rip currents

Watch Will Welbourn explain what causes waves, why they break at a specific depth, and how rip currents form, behave, and can be recognised from the beach or a dive boat.

What Causes Waves

The primary cause of waves is wind. When you see waves on the ocean, wind is almost certainly the cause. Waves can also be generated by seismic activity — tsunamis caused by underwater earthquakes or landslides — but these are rare. For exam purposes, and in everyday diving, waves mean wind.

Why Waves Break

Water particles inside a wave move in a circular path. Roughly one third of that circle extends below the waterline. As a wave approaches shore and the water gets shallower, the bottom of that circle starts dragging along the seabed. The wave loses stability and breaks.

The breaking point A wave breaks when the water depth below it is approximately 1.3 times the wave's height. At that depth, the seafloor interrupts the bottom of the circular water motion and the wave can no longer maintain its form.

Rip Currents

Rip currents are narrow, fast-moving currents that flow away from shore through the surf zone. They are sometimes called undertow or rip tides — but the correct term is rip current.

Property Typical values
Width 50–100 feet
Extent offshore 100 yards or more
Speed Can exceed 5 mph — faster than an Olympic swimmer

How a rip current forms

Waves continuously push water toward the beach. That water has to go somewhere — it cannot keep piling up on the shore. It runs sideways along the beach (the feeder current), finds the path of least resistance — a channel, a gap in a sandbar, or a break in a fringing reef — and flows seaward through it. As it goes, it erodes sand and deepens the channel, which strengthens the rip further.

Roatan context — Blue Channel and Spooky Channel Both are gaps in the fringing reef. On days with significant wave action breaking over the reef, water is being pushed into the lagoon and will escape seaward through those channels. Combine that with an outgoing tide and you can expect a strong current. Always assess wave conditions before diving channel sites.

When rip currents form

  • Waves only need to be 2–3 feet to generate a rip — they do not need to be large
  • They often occur on calm days following a storm, not only during bad weather
  • They are usually strongest near low tide but can form at any tidal state
  • Common where sandbars are present — rips form at breaks or channels in the bar
Exam trap — terminology Undertow and rip tide are common terms but both are incorrect. The proper term is rip current. If a question uses "undertow" or "rip tide" as an answer option alongside "rip current", the latter is always the correct choice.

How to recognise a rip current

  • A line of turbid (discoloured) or foamy water moving seaward
  • An area where waves are not breaking, while waves break on either side
  • Foam, seaweed, or debris being carried offshore
  • Much easier to spot from an elevated position — a dune, lifeguard tower, or dive boat
Note for your exam A rip current can be recognised as a line of turbid or foamy water moving seaward.