Rip Currents - Rivers Through The Surf
Rip Current Formation
Most waves are formed by wind on the water. Sea waves usually
result from storms, often hundreds of miles from shore. Waves are not
all equal in size. Sometimes a group of larger waves comes ashore one
after another. This is known as a "set" of waves.
When waves break, water is pushed up the slope of the shore.
Gravity pulls this water back toward the sea. If it converges in a
narrow, river-like current moving away from shore, it forms what is
known as a rip current.
Rip currents can be 50 feet to 50 yards or more wide. They can
flow to a point just past the breaking surf (the surfline) or
hundreds of yards offshore. Some 80% of rescues by lifeguards at
America's surf beaches are due to persons being caught in rip
currents.
Rip currents may pull continuously, but they can suddenly
appear or intensify after a set of waves, or when there is a breach
in an offshore sandbar. Longshore currents, inshore holes, and other bottom conditions
contribute to the formation of rip currents. Inshore holes and
sandbars can also greatly increase the danger of spinal injury.
Rip Current
Survival
The sea is a wonderful playground, but you must respect its
power. Learn to swim and consider participating in a junior lifeguard program. When
swimming, choose an area protected by lifeguards. If you are not a
strong swimmer, go no further than knee deep. If you decide to swim,
check the conditions first to identify any dangerous currents. Ask a
lifeguard for assistance.
You can sometimes identify a rip
current by its foamy and choppy surface. The water in a rip
current may be dirty (from the sand being turned up by the current).
The water may be colder than the surrounding water. Waves usually do
not break as readily in a rip current as in adjacent water.
If caught in a rip current, try to relax. A rip current is not
an "undertow" -- it will not pull you under. Do not try to swim
against the current as this is very difficult, even for an
experienced swimmer. If you can do so, tread water and float. Call or
wave for assistance. You can also try to swim parallel to shore until
you are out of the current, then swim directly toward shore.
Longshore
Currents
The same forces which cause rip currents also cause longshore
currents. These currents are most evident when waves hit the shore at
an angle. This tends to cause the water to be pushed along the beach
away from the direction of the oncoming waves. Usually, longshore
currents are less hazardous than rip currents because they move along
the shore, not away from the shore, but they can knock children and
weaker adults off their feet. More importantly, longshore currents
can feed and increase the power of rip currents. In other words, the
longshore current may move along the shore, then turn offshore to
become a rip current.
Inshore
Holes
Variable wave conditions, particularly seasonal changes in wave
patterns, can create unevenness in the ocean bottom. This includes
sandbars and sudden deep spots, called inshore holes. They can
surprise waders, who suddenly find themselves over their heads. They
can also create channels in the bottom, which concentrate and greatly
intensify the power of rip currents. At any beach with uneven bottom
conditions or obvious sandbars, a higher level of caution should be
used.
Safety
Tips
USLA has published a list of safety
tips. We recommend you follow all of them to ensure maximum
safety in the water.
USLA thanks the California State Lifeguards
and the Trauma Research and Education Foundation for their assistance
with this information.
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