- Low pressure which leads to a rise in sea level. Progressive waves move along the sea surface. Waves originate in the fetch area. Some of the greatest destruction comes from the storm surge or extreme high water levels due to the: Other Types of Progressive Waves Think of sloshing in bathtubs and or swinging in swing Whether an ocean current moves horizontally or vertically depends on its what? What was the trigger for this landslide? Refraction can be assessed by drawing wave orthogonals, imaginary lines perpendicular to the wave crest. Breaking is determined by wave steepness Marine terrace Wave Refraction (Figure 7-8a) There are two other notable types of progressive waves. SELECT ALL THAT APPLY. - Drag along the bottom. email prof. ] Standing waves (seiches) do not move horizontally. Standing waves can be dangerous due to the phenomenon of resonance. All of the following factors affect the probability of mass wasting EXCEPT: Which of the following mass wasting mitigation efforts is characterized by spraying reinforced concrete onto a slop surface? Slower speeds than surface waves because the density difference between water masses is less than between air and water. Interaction with the sea bottom. http://dusk.geo.orst.edu/oceans/waves.html, It is the energy of the wave, not its mass that is in motion. Click here for ANIMATION - Speed decreases Standing waves (seiches) do not move horizontally. Shallow Water Waves (Figure 7-4b) As waves enter shallow water their wavelength shortens and their height increases. Chapter 7 Summary depending on the slope of the bottom As waves enter shallow water: Constructive wave interference occurs when several wave crests or troughs coincide. Node = Fixed Point, Antinode = maximum displacement (Figure 7-11) A. a cave in a limestone They are stationary and It is due to: This area is characterized by a "confused" sea state with extensive wave interference. labs | What happens to the wave train because of wave dispersion? As waves enter shallow water their wavelength shortens and their height increases. Breaking is determined by wave steepness - Differential speed along the crest. In shallow water their length shortens and their height increases dramatically. Wave energy is focused where the lines converge. Wave height/wave length. Chapter 7 Summary In shallow water their length shortens and their height increases dramatically. They were principally triggered by __________. Period of wind or tides approximate the natural period of oscillation of the basin. I need help with the attached lab.. What type of a stream pattern is similar to the pattern formed by tree branches? The crests build up and the troughs build down. 239 In shallow water, the sea bottom transforms the wave's properties. Longer wavelength waves travel faster than shorter ones and move ahead of them in a wave train. Storm Surges Wave Refraction (Figure 7-8a) - Persistent onshore winds. It is wave energy not water molecules that moves across the sea surface. In the open ocean they have short heights, long wavelengths (>100 km), and long periods. email prof. ] A. shallow water on the seafloor causes waves to rise up Constructive wave interference occurs when several wave crests or troughs coincide. [ home port | Transformation of Shallow-water Waves (Figure 7-7b) Waves affect water to a depth equal to or less than one-half their wavelength. The orbits of the water molecules become elliptical. Think of sloshing in bathtubs and or swinging in swing Oscillate back and forth about a node i.e., a fixed point. Waves are disturbances that are generated on or beneath the sea surface. Seas, swell, and surf are progressive waves. Form when winds blow in one direction which causes water to pile up at one end of a basin. A jetty may have bad consequences for beach nourishment. The most damaging effect of storms is not necessarily the waves alone, but the waves in combination with storm surge (elevated sea level), created by the winds which pile water up along the shore. Surfing Video: Condition Black In shallow water, the sea bottom transforms the wave's properties. Standing Waves Seas, swell, and surf are progressive waves. B. flowing well Slower speeds than surface waves because the density difference between water masses is less than between air and water. Shallow-water Wave Transformations Some of the greatest destruction comes from the storm surge or extreme high water levels due to the: lectures | Which feature of a wave is most important in order to understand the wave base of a wave's motion? Destructive Waves (Figure 7-6c) It is the energy of the wave, not its mass that is in motion. B.. D. E. Which of these features signify a groundwater discharge area? In the open ocean they have short heights, long wavelengths (>100 km), and long periods. Life History of Ocean Waves (Cont.) Storm Surges O Angle that waves hit the shoreline O Fetch of the waves O The numberofwaves in the wave O Which type of tide results in the highest level of water? surf | This area is characterized by a "confused" sea state with extensive wave interference. What is the main difference between tidal flats/mud flats and lagoons? Bottom friction alters both the Oscillate back and forth about a node i.e., a fixed point. They have very long periods and very large heights. As waves enter shallow water their wavelength shortens and their height increases. Webaway Question 18 What persistent behaviorofwaves produces longshore drift? Waves are disturbances that are generated on or beneath the sea surface. D. jetty Wave height/wave length. Wave height/wave length. Internal Waves Seas, swell, and surf are progressive waves. Refraction can be assessed by drawing wave orthogonals, imaginary lines perpendicular to the wave crest. Which feature of a wave is most important to understand the energy of a wave? When the rate of discharge exceeds that of groundwater recharge, balances precipitation against evaporation and discharge. They have very long periods and very large heights. Some of the greatest destruction comes from the storm surge or extreme high water levels due to the: [ home port | Which type of tide results in the highest level of water? A drainage basin is also known as a watershed. B. Groin Internal waves which occur underwater and move along pycnoclines. Some of the greatest destruction comes from the storm surge or extreme high water levels due to the: Wave Refraction (Figure 7-8a) Answers: A. D. What persistent behavior of waves produces longshore drift? - Wind duration Which mass wasting type is very slow movement that can cause fences, retaining walls, and telephone poles to tilt downhill? D. spring - Wave form lectures | email prof. ] Life History of Ocean Waves Course Hero is not sponsored or endorsed by any college or university. Internal waves which occur underwater and move along pycnoclines. Slower speeds than surface waves because the density difference between water masses is less than between air and water. Constructive wave interference occurs when several wave crests or troughs coincide. A. tension - Drag along the bottom. Waves affect water to a depth equal to or less than one-half their wavelength. Wave Motions Storm Surges A. gaining stream Internal Waves Slower speeds than surface waves because the density difference between water masses is less than between air and water. Other Types of Progressive Waves [ home port | Storms affect shorelines in a variety of ways. surf | Tsunamis In shallow water, the sea bottom transforms the wave's properties. Transformation of Deep-water Waves: Dispersion (Figure 7-7a) The crests build up and the troughs build down. Two basic motions associated with an ocean wave: - Differential speed along the crest. The most damaging effect of storms is not necessarily the waves alone, but the waves in combination with storm surge (elevated sea level), created by the winds which pile water up along the shore. Tsunamis which are seismic sea waves. It is due to: Surfing Video: Condition Black Seas, swell, and surf are progressive waves. Water depths are less than 1/20 the wave length. http://dusk.geo.orst.edu/oceans/waves.html, Gravitational attraction of sun and moon Oscillate back and forth about a node i.e., a fixed point. Waves Break by Spilling Plunging, or Surging (Figure 7-9). Wave energy is focused where the lines converge. Standing Waves Swell - more regular waves beyond area of generation Tsunamis which are seismic sea waves. The orbits of the water molecules are circular. Standing waves can be dangerous due to the phenomenon of resonance. email prof. ] Progressive waves move along the sea surface. Slower speeds than surface waves because the density difference between water masses is less than between air and water. Standing Waves What would you expect to happen to the bedload and suspended load? [ home port | There are two other notable types of progressive waves. They occur when water masses slip over one another. http://dusk.geo.orst.edu/oceans/waves.html, They have very long periods and very large heights. A special case is a tsunami, a deepwater wave generated by a submarine disturbance with incredibly long wavelengths, high wave speeds, and very short wave heights, UNTIL they feel the bottom in shallow water! The speed at which waves approach the shore depends on sea floor and shoreline features and the depth of the water. As a wave moves toward the beach, different segments of the wave encounter the beach before others, which slows these segments down. As a result, the wave tends to bend and conform to the general shape of the coastline. depending on the slope of the bottom Rogue Waves? Which of these are considered to be the porosity of a material? Node = Fixed Point, Antinode = maximum displacement (Figure 7-11) - Destructive As waves enter shallow water: Waves Break by Spilling Plunging, or Surging (Figure 7-9) - Height increases Shallow Water Waves (Figure 7-4b) Tsunamis which are seismic sea waves. C. currents that bring water up always have a curved shape Storms affect shorelines in a variety of ways. 239 They are stationary and In shallow water their length shortens and their height increases dramatically. Dividing the wavelength by the wave period. http://dusk.geo.orst.edu/oceans/waves.html, - Destructive E. the curve of the run up of the beach Form when winds blow in one direction which causes water to pile up at one end of a basin. Chapter 7 Summary Some of the greatest destruction comes from the storm surge or extreme high water levels due to the: Wave Parameters (Figure 7-1a) This interference may be: Standing waves can be dangerous due to the phenomenon of resonance. Click here for ANIMATION - Persistent onshore winds. Some of the greatest destruction comes from the storm surge or extreme high water levels due to the: Some of the greatest destruction comes from the storm surge or extreme high water levels due to the: Destructive wave interference occurs when the crest of one wave coincides with the trough of another wave resulting in a cancellation. cracks, possibly with some vertical displacement, occur upslope, What are some clues that a proposed home site may be susceptible to landslide activity? As waves enter shallow water their wavelength shortens and their height increases. depending on the slope of the bottom - Differential speed along the crest. Sudden shifting of the ocean floor due to earthquakes, volcanic eruptions, and submarine slumping. Refraction can be assessed by drawing wave orthogonals, imaginary lines perpendicular to the wave crest. - Celerity Transformation of Shallow-water Waves (Figure 7-7b) D. Thistle Slower speeds than surface waves because the density difference between water masses is less than between air and water. They are stationary and. The orbits of the water molecules are circular. - Speed decreases A.don't change significantly B.travel faster C.get steeper D.grow smaller. Longshore drift is the movement of sediments along a coast by waves that approach at an angle to the shore but then the swash recedes directly away from it. The natural circular motion within the wave, Friction of the seafloor slowing waves, causing the crest to grow, How often does a full cycle of a tide occur? The size of surface waves depends on the speed and duration of the wind, and the fetch. Sudden shifting of the ocean floor due to earthquakes, volcanic eruptions, and submarine slumping. Why is the lunar or tidal day longer than the solar day? Which of these is a source of nonpoint pollution? It happens when waves approach the beach at an angle. Sudden shifting of the ocean floor due to earthquakes, volcanic eruptions, and submarine slumping. - Celerity In deep water most waves do not interact with the sea bottom and are called deep-water waves. Period of wind or tides approximate the natural period of oscillation of the basin. surf | - Low pressure which leads to a rise in sea level. Period of wind or tides approximate the natural period of oscillation of the basin. [ home port | Think of sloshing in bathtubs and or swinging in swing Life History of Ocean Waves (Cont.) Some of the greatest destruction comes from the storm surge or extreme high water levels due to the: http://dusk.geo.orst.edu/oceans/waves.html, In shallow water their length shortens and their height increases dramatically. [ home port | Breaking is determined by wave steepness. Click here for ANIMATION 17.0 mol of germanium, b. Waves Break by Spilling Plunging, or Surging (Figure 7-9) - Wave form Standing waves can be dangerous due to the phenomenon of resonance. Oscillate back and forth about a node i.e., a fixed point. When this value is about 1/7, waves begin to break. Standing waves (seiches) do not move horizontally. Shore breakers (surf) are collapsing waves. Refraction can be assessed by drawing wave orthogonals, imaginary lines perpendicular to the wave crest. Storm Surges Shallow Waves Affected by Bottom Life History of Ocean Waves (Cont.) Wave energy is focused where the lines converge. Node = Fixed Point, Antinode = maximum displacement (Figure 7-11) - Low pressure which leads to a rise in sea level. The result is amplification of the wave size which can lead to flooding. A trellis drainage pattern would be commonly associated with ________. - Destructive A special case is a tsunami, a deepwater wave generated by a submarine disturbance with incredibly long wavelengths, high wave speeds, and very short wave heights, UNTIL they feel the bottom in shallow water! In shallow water, the sea bottom transforms the wave's properties. Some of the greatest destruction comes from the storm surge or extreme high water levels due to the: Which of the following is an example of a coastal hazard? Which feature of a wave is most important to understand the energy of a wave? The most damaging effect of storms is not necessarily the waves alone, but the waves in combination with storm surge (elevated sea level), created by the winds which pile water up along the shore. All following actions can help mitigate the risk of mass wasting EXCEPT: building a house on top of a cliff to compress the material beneath it, When a landslide damn a river the resulting flooding can be deadly, Which of the following forces are NOT involved in a mass sliding down a slope, The shape of the water molecule is unique with two hydrogen ions bonded to the side of the oxygen ion. Progressive Wave Types D. tombolo Simply put, wave size increases as the strength and duration of the wind, and distance over which it blows increases. Wave Motions What forces are involved in a mass sliding down an inclined plane? - Low pressure which leads to a rise in sea level. Surf - waves that have reached the coast, grow in height, and break Wave height/wave length. Wave Motion with Depth (Figure 7-3a) (Figure 7-6b) Slower speeds than surface waves because the density difference between water masses is less than between air and water. Also, waves do not typically reach the beach perfectly parallel to the shoreline. Rather, they arrive at a slight angle, called the angle of wave approach. When a wave reaches a beach or coastline, it releases a burst of energy that generates a current, which runs parallel to the shoreline. This type of current is called a longshore current. -The natural circular motion within the wave The result is amplification of the wave size which can lead to flooding. Formula on pg. The size of surface waves depends on the speed and duration of the wind, and the fetch. Waves affect water to a depth equal to or less than one-half their wavelength. Sea - irregular waves in the area of generation In shallow water, the sea bottom transforms the wave's properties. The size of surface waves depends on the speed and duration of the wind, and the fetch. F. polarity Waves Entering Shallow Water Node = Fixed Point, Antinode = maximum displacement (Figure 7-11). Form when winds blow in one direction which causes water to pile up at one end of a basin. Wave Motion with Depth (Figure 7-3a) 239 Chapter 7 Summary Tsunamis which are seismic sea waves. The orbits of the water molecules become elliptical. Which part of a coastal area is always under water? Tsunamis which are seismic sea waves. They have very long periods and very large heights. Which type of tide results in the highest level of water? They occur when water masses slip over one another. Tsunamis which are seismic sea waves. Life History of Ocean Waves (Cont.) In the open ocean they have short heights, long wavelengths (>100 km), and long periods. It is wave energy not water molecules that moves across the sea surface. Shore breakers (surf) are collapsing waves. Internal waves which occur underwater and move along pycnoclines. Sea - irregular waves in the area of generation Other Types of Progressive Waves email prof. ] Period of wind or tides approximate the natural period of oscillation of the basin. 3.2271010. An aquifer should have which of the following qualities: choose three. They occur when water masses slip over one another. Standing waves (seiches) do not move horizontally. - Low pressure which leads to a rise in sea level. The crests build up and the troughs build down. Waves which interact with the sea floor are known as shallow-water waves. Oscillate back and forth about a node i.e., a fixed point. This leads to wave refraction and waves collapse forming surf (breakers). The type of wave generated by wind is determined by: Waves are disturbances that are generated on or beneath the sea surface. http://dusk.geo.orst.edu/oceans/waves.html, - Wavelength shortens The result is amplification of the wave size which can lead to flooding. Shore breakers (surf) are collapsing waves. Standing Waves Freshwater influx from rivers _________ salinity and, therefore, _________ the density of seawater. B. drinkable Why build them in the first place? C. it runs off B. nearby stream There are two other notable types of progressive waves. During the spring tide, the Moon, Sun, and Earth would exist in a same straight When a wave breaks at a more acute (steep) angle on a beach, encounters a steeper beach slope, or is very Swell - more regular waves beyond area of generation Waves Break by Spilling Plunging, or Surging (Figure 7-9) Node = Fixed Point, Antinode = maximum displacement (Figure 7-11) Longshore currents are affected by the velocity and angle of a wave. When a wave breaks at a more acute (steep) angle on a beach, encounters a steeper beach slope, or is very high, longshore currents increase in velocity. Conversely, a wider breaking angle, gentler beach slope, and lower wave height slows a longshore currents velocity. Which of the following are formed by wave erosion? Standing waves can be dangerous due to the phenomenon of resonance. moves heat around the planet, distributing it, Which of these features are found on emergent coastline, with a relative falling sea level? A special case is a tsunami, a deepwater wave generated by a submarine disturbance with incredibly long wavelengths, high wave speeds, and very short wave heights, UNTIL they feel the bottom in shallow water! Motion of Water Particles Beneath Waves (Figure 7-3b) choose two. Chapter 7 Summary when the rate of discharge exceeds that of recharge. A special case is a tsunami, a deepwater wave generated by a submarine disturbance with incredibly long wavelengths, high wave speeds, and very short wave heights, UNTIL they feel the bottom in shallow water! Answers: A. C. D. The number one factor responsible for triggering landslides is the ____________. Storms affect shorelines in a variety of ways. Storm Surges Progressive Waves email prof. ] Period of wind or tides approximate the natural period of oscillation of the basin. - Wavelength shortens Some of the greatest destruction comes from the storm surge or extreme high water levels due to the: Internal waves which occur underwater and move along pycnoclines. It is the energy of the wave, not its mass that is in motion. The compact was made in a year of high flow and based allocations on specific volumes and did not consider growth/drought. Which of the following states would have the lowest risk for mass wasting events? It forms there because: CO2 from the atmosphere dissolves in water droplets in clouds from which precipitation falls. Click here for ANIMATION, When wave passes, no net displacement of water. Standing Waves Other Types of Progressive Waves Standing Waves In the open ocean they have short heights, long wavelengths (>100 km), and long periods. Resonance Transformation of Deep-water Waves: Dispersion (Figure 7-7a) lectures | Slower speeds than surface waves because the density difference between water masses is less than between air and water. This may be easier to, Spits, bars, berms, barrier islands, and other features related to longshore drift are ultimately the result of what? Longshore drift is simply the sediment moved by the A special case is a tsunami, a deepwater wave generated by a submarine disturbance with incredibly long wavelengths, high wave speeds, and very short wave heights, UNTIL they feel the bottom in shallow water! E. Rock towers The most damaging effect of storms is not necessarily the waves alone, but the waves in combination with storm surge (elevated sea level), created by the winds which pile water up along the shore. choose three. Waves Break by Spilling Plunging, or Surging (Figure 7-9) All of the following are ways in which sedimentary rocks form EXCEPT: A mixture of Fe2O3Fe_2O_3Fe2O3 and FeOFeOFeO was found to contain 72.00% FeFeFe by mass. An ocean wave is an undulation of the sea surface. http://dusk.geo.orst.edu/oceans/waves.html, Oscillate back and forth about a node i.e., a fixed point. Bending of the wave crest as waves enter shallow water. Destructive wave interference occurs when the crest of one wave coincides with the trough of another wave resulting in a cancellation. Transformation of Shallow-water Waves (Figure 7-7b) - Wave form Think of sloshing in bathtubs and or swinging in swing What percentage of freshwater is groundwater? labs | depending on the slope of the bottom Storms affect shorelines in a variety of ways. The ridge and valley province of the Appalachian Mountains is a good palce to find an example of a trellis drainage pattern. Form when winds blow in one direction which causes water to pile up at one end of a basin. In shallow water their length shortens and their height increases dramatically. Fetch of the waves C. Rogue Waves? Click here for ANIMATION D. nearby cliff (with crescent shapes indicating scarp) They are stationary and Progressive Waves Shallow water on the seafloor causes waves to rise up. As waves enter shallow water their wavelength shortens and their height increases. Resonance Moving sand _____ causes surface currents, _____ causes In the open ocean they have short heights, long wavelengths (>100 km), and long periods. They occur when water masses slip over one another. The type of wave generated by wind is determined by: Materials on a slope tend to move downslope when the _____ force exceeds the _____ force. surf | Seas, swell, and surf are progressive waves. - Destructive F. car exhaust in the winter Form when winds blow in one direction which causes water to pile up at one end of a basin. Wave Orthogonals (Figure 7-8) B. tidal flat Waves originate in the fetch area. Seas, swell, and surf are progressive waves. - Destructive Refraction can be assessed by drawing wave orthogonals, imaginary lines perpendicular to the wave crest. Shore breakers (surf) are collapsing waves. Internal waves which occur underwater and move along pycnoclines. A special case is a tsunami, a deepwater wave generated by a submarine disturbance with incredibly long wavelengths, high wave speeds, and very short wave heights, UNTIL they feel the bottom in shallow water! Slower speeds than surface waves because the density difference between water masses is less than between air and water. WebLongshore currents are affected by the velocity and angle of a wave. Waves affect water to a depth equal to or less than one-half their wavelength. Surfing Video: Condition Black Chapter 7 Summary Other Types of Progressive Waves Node = Fixed Point, Antinode = maximum displacement (Figure 7-11) Resonance surf | email prof. ] Wave Refraction (Figure 7-8a) Standing Waves Standing waves can be dangerous due to the phenomenon of resonance. - Constructive Answers: A. F. What is the main difference between tidal flats/mud flats and lagoons? Shallow-water Wave Transformations Water is most dense 4 degrees above its freezing point. This emergent coastal feature is formed when a rock, sea stack, or small island become connected to the main shore by the deposition of sand behind it, due to wave refraction? When this value is about 1/7, waves begin to break. Wave energy is defocused where the lines diverge. Shore breakers (surf) are collapsing waves. Destructive Waves (Figure 7-6c) What persistent behavior of waves produces longshore drift? Period of wind or tides approximate the natural period of oscillation of the basin. - Wavelength shortens D. exactly 24 hours http://dusk.geo.orst.edu/oceans/waves.html, http://dusk.geo.orst.edu/oceans/waves.html. Sudden shifting of the ocean floor due to earthquakes, volcanic eruptions, and submarine slumping. Storm Surges It is due to: This interference may be: lectures | Standing waves (seiches) do not move horizontally. Refraction can be assessed by drawing wave orthogonals, imaginary lines perpendicular to the wave crest. Seas, swell, and surf are progressive waves. What Causes Waves? The size of surface waves depends on the speed and duration of the wind, and the fetch. In deep water most waves do not interact with the sea bottom and are called deep-water waves. Oscillate back and forth about a node i.e., a fixed point. In shallow water their length shortens and their height increases dramatically. C. playa Surf - waves that have reached the coast, grow in height, and break Slower speeds than surface waves because the density difference between water masses is less than between air and water. A. shoreface/nearshore Internal waves which occur underwater and move along pycnoclines. email prof. ] They are stationary and The crests build up and the troughs build down. Other Types of Progressive Waves Standing waves can be dangerous due to the phenomenon of resonance. Rogue Waves? They have very long periods and very large heights. Radial C. Trellis D. Rectangular, Your return customer. - Persistent onshore winds. lectures | Internal waves which occur underwater and move along pycnoclines. They occur when water masses slip over one another. - Wave form What landform would this create? Interaction with the sea bottom. Some of the greatest destruction comes from the storm surge or extreme high water levels due to the: F. Sinkholes Standing waves (seiches) do not move horizontally. (Figure 7-6b) In deep water most waves do not interact with the sea bottom and are called deep-water waves. The most damaging effect of storms is not necessarily the waves alone, but the waves in combination with storm surge (elevated sea level), created by the winds which pile water up along the shore. WebOblique incoming wind squeezes water along the coast, and so generates a water current which moves parallel to the coast. - Persistent onshore winds. The most damaging effect of storms is not necessarily the waves alone, but the waves in combination with storm surge (elevated sea level), created by the winds which pile water up along the shore. This leads to wave refraction and waves collapse forming surf (breakers).
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