Coastal Processes Chapter 13 Waves Beaches And Coastal Erosion Rivers of Sand 1 Wave Processes and Shore Erosion Waves form as wind blows over the ocean surface Waves increase in size with the following factors greater wind velocity greater amount of time the wind blows greater fetch Refer to pages 356 360 2 Wave Processes and Shore Erosion Wave height and wavelength increase with increasing energy wave height the vertical distance from low point trough to high point crest wavelength the horizontal distance from one crest to the next crest Refer to pages 356 360 3 Wave Processes and Shore Erosion In deep water the wave form itself moves but the water does not have net forward motion instead the water travels in circlular orbits right The circular motion of the water fades downward to a depth equal to half the wavelength called wave base below Refer to pages 356 360 4 Wave Processes and Shore Erosion At a water depth equal to or less than half the wave length the waves begin to feel bottom The crest of the wave moves forward as the base drags on the bottom This causes the waves to bunch up wavelengths decrease and grow taller wave heights increase Refer to pages 356 360 5 Wave Processes and Shore Erosion Eventually the waves oversteepen causing them to tumble toward the shore or break and the water moves landward Refer to pages 356360 6 Beaches Beaches are accumulations of sand or gravel supplied by Sea Cliff Erosion and by River Transport of Sediment to the Coast The sand and gravel supplied to the coast is then moved by wave action 7 Wave Refraction and Cliffed Coasts Refer to pages 361 362 Wave refraction is the bending of waves to conform to the shape of the coastline Wave refraction concentrates wave energy on headlands and deposits the products of that erosion in bays ultimately straightening the coastline 8 Erosional Remnants of Cliffed Coastlines Eroded by Wave Refraction 9 Longshore Drift Refer to pages 361 362 The gradual migration of sand along the shoreline Sand grains are pushed up onto the beach in the direction of wave travel Gravity pulls it back directly down the slope of the beach We measure longshore drift by the volume of sand moved in cubic meters per year Longshore drift in parts of coastal California averages 750 000 m3 year or the equivalent of 2 000 10m3 dumptrucks per day Longshore drift along the East Coast averages 75 000 m3 year 10 Seasonal Beach Winter Summer Beach Profile Refer to pages 363 365 11 Storm Response Loss of Sand from the Beach Refer to pages 364 367 Larger waves and storm surge erode sand from the shallow portion of the beach and transport much of it just offshore Much of the eroded material comes from the surface of the beach eroding it to a flatter profile Top This beach in California was eroded by waves during a storm event Right But was naturally rebuilt by 1998 12 Barrier Islands Barrier islands are long narrow offshore deposits of sand that parallel the coast line separated from the main land by a shallow sound bay or lagoon They are the products of dynamic coastline processes erosion deposition longshore drift and wind transport 13 Barrier Islands Barrier islands are often found in chains along the coast line and are separated from each other by narrow tidal inlets A baymouth barrier is a barrier beach that is attached at both ends to the mainland and backed by a bay or lagoon A spit is a protrusion or linear beach extending from the mainland 14 Barrier Islands Most barrier islands in North America are along the Atlantic Coast The photograph at left shows the barrier islands off of Long Island and New Jersey These islands extend almost continuously south to 15 Georgia Barrier islands are places of change and motion Longshore drift moves sand from one beach to another Islands grow and shrink depending on the amount of sediment available dams sand mining hardening Sea level rise causes them to erode and to shift toward the mainland over time An island that is migrating toward the mainland is termed retrograding In most cases an island that is retrograding undergoes a process known as island rollover 16 Barrier islands are places of change and motion Two forms of evidence that show an island is rolling over are washovers and exposed marsh mud and oyster shells on the beach 17 Barrier islands are places of change and motion This figure shows how Hog Island Virginia has changed over the past 150 years as a result of hurricanes and wave erosion The dashed lines show the former shorelines of the island Entire towns such as the once thriving community of Broadwater have disappeared into the ocean as the barrier has shifted toward the mainland 18 Barrier islands are places of change and motion Refer to pages 367 371 Barrier islands maintain their equilibrium profile by migrating shoreward with rising sea level Because many barrier islands are now covered with buildings the island cannot migrate but is progressively eroded 19 20 Seawalls Seawalls are structures constructed parallel to the coastline and are generally used as a last resort to protect property landward of an already eroded small beach They may be constructed of concrete large stones riprap wood or other material and are essentially built to repel the sea 21 Seawalls Refer to pages 374 376 Seawalls accelerate erosion as water hits the sea wall with high energy and retreats with high energy The beach narrows and becomes steeper and the water in front of the seawall deepens As a result bigger waves approach closer to shore hastening erosion and removal of the beach Seawalls require costly repair Large storm waves can overtop sea walls and cause flooding 22 Sea Cliffs Some shorelines particularly on the western coast of the U S are dominated by sea cliffs rather than beaches The tops of these cliffs form prime real estate But sea cliffs are subject to erosion by both wave undercutting and mass wasting Refer to pages 371 373 23 Groins Refer to pages 374 376 Groins are built to trap sand being carried by longshore drift and build up the beach updrift of the structure Unfortunately these structures starve downdrift beaches of sand and erosion on those beaches is accelerated The only way to save downdrift beaches is to construct more groins and therefore groins tend to multiply into groin fields 24 Jetties Refer to pages 374 376 Jetties are built to maintain an open inlet by blocking the movement of sand by longshore drift The sand builds up on the upcurrent side of the jetties and
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