Natural Hazards Ch 15 Waves, beaches, coastal erosion
We build various kinds of structures in an attempt to save our beaches and beach homes, unintended effect of reducing sand migration
- jetties around a marina - seawall - rip rap - groins -breakwaters
The power of waves are in circular motion?
- largest at surface - no water movement happens below 1/2 of the wavelength
Longshore drift of beach sediments often end in submarine canyons
- move particles down the beach in a river fashion, gets stuck down the cliffs and into the deep ocean, river of sand then disappears the sandy beach is gone
Material moves along a beach, grain of sand on the beach based on the wave motion what direction would a grain of sand move?
- wherever direction the wave is approaching shore - when water goes back out it does not go back out at an angle, moves backward along the same pattern
Beach Erosion <----Sand supply is short because:
-dams trap sand -sand mining for construction use
reasons for sand loss
-rip currents -wind blows it inland to make dunes -drift into inlets that cross barrier islands forcing humans to dredge it -carried away by hurricanes
Wave Energy equation
0.125rgH^2L - r = water density - g = gravity - h = wave height - l - wavelength
beach growth occurs by:
1. due to coarser sand or gravel, much of the water soaks quickly into the ground rather than flowing back offshore over the surface; thus, less sand or gravel is eroded from the beach. 2. small waves tend to leave more of their sand onshore.
Equation of wave velocity in deep water
1.2L^1/2 L - wavelength
Replenishment Issues:
1.Expensive: Localities pay about 5% of cost and the remainder is payed by the state and federal governments. 2. Uncertain Durability: Projected up to 20 years but typically only lasts a couple 3. Sand supply: Florida is running out of sand to supply for beaches and we could start to talk from other sources such as the Bahamas 4. extra sand naturally migrates somewhere causing another issue
equation of wave velocity in shallow water
3.1D^1/2 D = water depth
waves that are 2x as high have _____ the energy
4x
Barrier islands
A near-shore, coast-parallel island of sand built up by waves and commonly capped by windblown sand dunes. Also called a barrier bar - some protection to coastline - coastal lagoon forms on landward side that is usually below sea level
Result of Groins
A zig-zag beach where the sand is carried on one side of the barrier and eroded on the next because the current pushes the sand until it hits one of the groins then a new current begins at the next barrier.
To what depth of water do waves commonly move sand?
About 10 meters
Limiting Development
Adjust controls on building via zoning. Measures E-10 to E-60 and creates a graduated system. E-10:Imminent hazard, E-30: Intermediate zone, E-60: Longer term hazards. Limits property owners rights, property damage, and relief needs.
Replinshment
Also referred to as 'Beach Nourishment'. Manually move sand to beaches and you pump from offshore or other beach zones. It involves joint projects from localities, states, and corps of engineers.
Barrier Islands
Are not permanent; develop where the landward-steepening beach profile is steeper than the general slope of the coast. Wind blows sand shoreward into dunes
Which of the following evidence does NOT indicate that a barrier island migrated landward?
Barrier island beaches are now more easily eroded than they were one hundred years ago.
Where does beach sand NOT originate?
Continental shelf as much as 50 km offshore
Littoral Cells
Develop when there are multiple outlets for sand
Natural Island Migration
Driven by changes in sea level; a rise in sea level causes waves to push the sand backwards which creates the barrier island to shift
Why are ocean waves generally larger than those on lakes?
Fetch length is much longer in the ocean.
East Coast Drift
Gentle offshore slopes: gently breaking waves; relatively slow sand loss causes large beach zones. coarser materials
Breakwaters
Hard structures parallel to the beach. Purpose is to intercept waves before shoreline
Seawalls
Hard structures parallel to the beach. They save properties and are built behind beach to protect property.
Groins
Hard structures perpendicular to the beach are used to trap the sand from moving with the longshore drift.
Jetties
Hard structures perpendicular to the beach. Purpose is to protect an inlet; not allow any boats to come from the sound side to the ocean side.
What are the three basic types of hazards? and what are they triggered by?
Hurricanes, typhoons, nor'easters; day-to-day processes
Beach Replenishment/Nourishment
Involves replacing sand on a beach, an expensive proposition that needs repetition at intervals
Result of Jetties
Jetties cause erosion on the backside and pile up of sand on either side of the barriers depending on the current
West Coast Drift
Keep offshore slopes: steeply breaking waves; relatively quick sand loss causes small beach zones
Consequence of the current
Long-shore current and waves push water towards shore and eventually the build up gets flushed out which causes a rip current.
Result of breakwaters
Longshore drift stops behind the barrier and you get a pile up of sediment
Why does sea level rise during a near-shore storm?
Low atmospheric pressure of the storm permits sea level to rise.
Lake Shorelines
Many lakes large enough for the same processes; they have a greater stability expectation and less tolerance for changes
Dune Stabilization
Protecting dune lines as a storm buffer by the use of sand fences and vegetation
Why are inlets through barrier bars or barrier islands not closed by longshore drift of sand?
Rapid flow of water back and forth through the inlet as tides rise and fall keeps it clear.
The three types of adapting:
Replenishment, dune stabilization, and limiting development
Rip Current
Rip Current
Without outlets what would happen to the beaches?
Sand gets carried along the beach for great distances
Beach erosion prevention or stopping the longshore drift of sand includes?
Seawalls; groins; jetties; breakwaters
wave refraction
Slowing and bending of progressive waves in shallow water.
What is sea cliff erosion determined by?
Strength of the rock; wave height; sea level; precipitation; resulting in amplified erosion during storms
possible solution
The cost of moving buildings may be high, but it is less than the continuing long-term cost of maintaining beach-hardening structures that tend to destroy their beaches or of continually bringing in thousands of tons of sand that get removed by following storms.
Beach Stabilization (Interfering with drift)
Trying to keep the beach in place because sand movement causes erosion which can damage beach front property
What is the ULTIMATE cause of coastal hazards?
Us; population density is increasing faster at coastal areas then any other area
Why do waves not break in the open ocean?
Water in deep-water waves does not move forward with the wave; it moves in a circular motion.
Long-shore Current
Waves approaching the beach at an angle push sand parallel to shore
Why does the beach slope under water become steeper near shore?
Waves in shallow water drag on the bottom, so they lose energy and need a steeper slope to move the sand.
equilibrium profile
Whether or not the sediment moves shoreward depends on the balance (equilibrium) between shoreward bottom drag by the waves, size of bottom grains, and downslope pull by gravity
What effects the rip current and how does it effect it?
Wind; no wind causes no rip current or riptides and lots of wind causes large rip currents
rip rap
a useless mitigation effort that requires Coarse rock piled at the shoreline in an attempt to prevent wave erosion of the shore or destruction of a nearshore structure. can do more harm than good in long run
Longshore drift
angled waves pushes a river of sand along the shore near the beach
what causes a wave to break
bottom of the circular particle motion drags on the bottom, slowing it - the top continues to move forward
waves created by storms:
can lead to waves either combining, forming rogue waves, or cancelling each other out
Sand on the beach is made of?
clear, glass like, quarts come from particular rock types not found in the ocean, quarts come from rivers so the way sand gets through the ocean is through rivers
How does sediment get to the coasts
cliff erosion, bottom of the ocean , waves and rivers
beach hardening, structures built to protect properties, backfires by
contributing to further erosion
Rivers carry sediment, it is trapped when
dams are built
Energy is associated with
density
dunes disappearing bc:
development
Wave refraction focuses
erosion
Longer wavelengths moves?
faster
wavelength and depth relationship
feeling bottom when depth = .5 wavelength. shorter wavelength means the depth at which bottoming occurs is also smaller. this causes the wave to grow tall
two factors that increase wave height
fetch and length of time the wind blows
Why does removal of logs and rocks from a beach endanger the sea cliffs behind them?
force of wave is softened by the logs and rocks acting as natural barriers
When wave hits the bottom of the ocean it deforms?
goes from circle to oval, changes shape and slows down
shore profile?
grain size strongly controls the slope of the beach
You cannot own property past the
high water mark, federal government owns from the high water mark outwards
Seawalls are built to?
keep ocean from moving backward and eroding the land, dump sediment along the base of the seawall
jetties are built to
keep out waves and keep the sand from making it too shallow. Made to protect navigation channels and require freq dredging
loss of sand occurs from
large waves of storms and high tides removing sand from the surface of the shallow portion of the beach and from the sea side of dunes the waves break against
fetch
length of water surface over which the wind blows
storm surge
local rise in sea level from low atmospheric pressure in the midst of a storm - high winds push them forward and can cause massive erosion
Groins protruding into the surf stop?
longshore drift of sand
wave energy is proportional to
mass of moving water
Dunes
mounds of wind-deposited sand -removing dunes puts buildings at risk
typical wave motion offshore
moves in circular motions, staying in place. Floating objects move up and down. Not dangerous
Breakwaters are built>
offshore and parallel to the shore, causing depostion in the protected area behind the barrier
Waves break against a seawall, stirring?
offshore sand and causing erosion
Where will erosion occur at highest
on headlands
As the wave drains back into the sea the water moves?
perpendicular to the waters edge
Shape is related to
process
Wave velocity in shallow water is
proportional to square root of water depth
Wave velocity in deep water is ?
proportional to the square root of wavelength
Homeowners placing large boulders in front of house for protection is bad bc:
protection is temporary. big waves reflect off the boulders, washing away the beach sand in front and steepening the remaining beach. Eventually, the boulders will slide into the wave-eroded trough, leaving the homes even more vulnerable
Wave energy doubles wave heigh _______ energy
quadruples
Edge of landscape submerged as sea level
rises
Barrier bars move inland with
rising sea level picks up particles and waves push it forward and deposit it further inland
how does on particle of water in a wave zone move
rolling in a circular motion, top of the circle moving in the direction of wave motion
Massive Corps Of engineers Beach replenishment project
sand and water slurry is pumped from up coast in 30 inch pipes - heavy earthmoving equipment spread the sand
sand will get trapped inside barriers?
sand builds up inside the groins, building up on upstream side makes the beach bigger and wider
beaches change with seasons
sand in summer and gravel and boulders in winter
small waves tend to leave more
sand onshore
Headlands
separated by shallower sandy bays that reach into deeper water, energy focuses against headlands
shore profile
slope of beach determined by grain size
A constant, mild onshore wind will produce waves with
smaller and shorter wavelengths.
Coarser grains need a
steeper slope to move in the surf
You should escape a ripcurrent by
swimming parallel to shore and then back to the beach
Long-shore Drift
the movement of sand along the beach. looping motion
Coast in Louisiana has muddy beaches because
the sediment is coming from the Mississippi river which carries a lot of mud
Hawaii doesnt have quart sand because
they dont have quart rocks so you get volcanic beaches, carbonate from reefs, green beaches caused by peridotite
Overtime the ocean will attempt to tear back the headlands because?
they will get eroded and positive inside and overtime the heandlands retreat and form a straight cliff
Breakers
water at the base of the wave cant move toward the beach - top of wave circles deformed moves ahead of base (rise up)
rip current
water constantly coming in at one place, going back out another place, almost creating a river - can be permanent at groins, jetties, and outcrops where water flowing against piles up and is forced to flow offshore along the structure
Shallower water, smaller waves, and coarser grains promote steeper slopes offshore
water that arrives here carrying sediment slows immensely and drops it onto the steep slow before reaching shore causing further steepening
Beach face forms by
wave action
Result of Seawalls
wave that hits erodes sand in front of wall. the beach narrows and gets steeper. water in front of barrier deepens and waves reach closer to chore b4 breaking. when the water in front of barrier gets deep enough the structure is undermined and fails
35 m high waves occur every year and develop where:
wave travel direction is opposite to a strong current direction such as off the tip of South Africa
building on a cliff is bad idea bc:
waves hitting rock face erode material and undermine the cliff. can cause a landslide
What causes waves
wind blowing across the water (contact between water and wind, air can drag the ocean with it)