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MOTION IN THE
   OCEAN
Waves, Tides, and Currents




       Chapter 16.2
Waves
   A disturbance which
    moves through or
    over the surface of a
    fluid

   Mostly caused by
    winds
     (Also earthquakes,
        volcanoes, grav.
    pull)

   Form of great energy
Wave Characteristics
   Parts of a Wave
       Crest = high point

       Trough = low point

       Height = vertical
        distance from crest to
        trough

    
        Wavelength =
        Horizontal distance
        between crest to crest
        or trough to trough
Wave period : time for 2 crests to pass fixed point (T) sec

Wave speed (C) : C = wavelength / T (m/s)
Wave steepness : H / wavelength
  When H / wavelength = 1/7 or angle at crest 120 or less =
     Breaker
Size of Wind Generated
                 Waves
   Depends on 3 things:
    
        Wind Speed
    
        Wind Duration (length of
        time wind blows)
    
        “Fetch” Extent of open
        water across which the
        wind can blow
Water Motion in Waves

   Water travels in vertical
    circular orbits

   Wave moves, particles don’t!
Importance of Waves
 Shaping
 Coastlines
     Erode cliffs
     Grind rock into sand


 Ecology
     Returns O2 to water
     Stir up food for filter
      feeders
Types of Waves
CHOP – Short period (back bays)

SWELL – Long period (boat rolls; seasickness)

SWASH – water up beach        BACKWASH – back down
TSUNAMI                   “TIDAL WAVE”

Caused by undersea quake or volcano
• Wavelength = ~150 mi.           Wave height = 6” – 1’
      Can NOT perceive in boat          Speed > 500 mph

Slows down to ~25 mph at shore; water builds up to ~65+ ft
Tsunami Waves
Creation of a Tsunami
Tides
   The rhythmic rise and
    fall of the ocean’s water

    High tide = rising, incoming
    tide, flow
    Low tide = receding, outgoing
    tide, ebb
    Slack tide = vertical movement
       stops
   Tides are very long,
    slow waves

       They have a wave
        period of 12 hours 25
        min

       Tidal day is 24 hours
        50 min

    
        NJ has 2 high and 2
        low tides daily
What Causes Tides?
1. Gravitational pull of
  sun & moon on Earth

• Moon closer, therefore
     > effect

• Like magnet, pulls water
       away from surface
       = TIDAL BULGE
2. Centrifugal Forces
                           • Bulge on opposite side
• Produced by motions of
                           because centr. force     >
Earth, sun, & moon
                           pull of moon
Types of Tides
•Spring Tide
      - Moon and sun are in direct
              line with one another
      - Results in unusually
      high tidal range
   -Tidal Range = vertical
   distance between high &
   low tides
     2x’s/month
   Neap Tide
       sun and moon are at
        right angles

    
        Pulls cancel each
        other out – causes a
        weak pull

       unusually low tidal
        range

       2 x’s / month
Spring vs. Neap Tides
Distance bet. Moon & Earth
Perigee Tides
  • Moon closest to earth, very high tides (causes
    flooding)
Apogee Tides
  • Moon farthest away from earth, very low tides
Types of Tides Continued
   Diurnal Tides
     
       1 high & 1 low / day
     
       Parts of Gulf of Mexico and Asia

   Semi-Diurnal Tides
     
       2 high & 2 low / day
     
       Atlantic coasts of North America and Europe

   Mixed
     2 high & 2 low / day (height varies)

     Pacific coast
Importance of Tides
• Expose & submerge orgs

 • Circulate water in bays &
 estuaries
 • Circulates food, wastes, etc
• Trigger spawning (grunion,
       horseshoe crab)
Currents
• What are currents?
  - “Rivers” of circulating water

• Causes
  - Wind
  - Rotating Earth
  - Density Changes
Surface Ocean Currents
• Broad, slow drifts; never
cross equator

• Wind generated; circular
      gyres
•   Coriolis Effect
- N. Hemis – clockwise; Right

    - S. Hemis – counterclockwise; Left
• Gulf Stream
     - N. Atlantic
   - Brings warm water
   from equator north along
   east coast of N. A.




-Sometimes form eddies –
circulating water that                  pinches
off from the                  current
MIGRATION             NAVIGATION




            WEATHER
Localized Surface Currents
Longshore Current.
  
      Flows parallel to shore; move sediment
RIP CURRENT
   - Caused by converging longshore currents
   - Very dangerous ; Red Flag
   - DO NOT fight rip current; swim parallel to shore to
          get out of channel
Deep Ocean Currents
Flow beneath surface; cross
    equator
Move North to South

   Separated from surface
    currents by boundary
    called a “Thermohaline”
    (diff in densities)
Importance Of Deep

    Upwelling Currents
    • Brings deep water to surf.
    • Circulates nutrients up
    • Moves plankton & larvae

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Motion in the Ocean: Waves, Tides and Currents

  • 1. MOTION IN THE OCEAN Waves, Tides, and Currents Chapter 16.2
  • 2. Waves  A disturbance which moves through or over the surface of a fluid  Mostly caused by winds (Also earthquakes, volcanoes, grav. pull)  Form of great energy
  • 3. Wave Characteristics  Parts of a Wave  Crest = high point  Trough = low point  Height = vertical distance from crest to trough  Wavelength = Horizontal distance between crest to crest or trough to trough
  • 4. Wave period : time for 2 crests to pass fixed point (T) sec Wave speed (C) : C = wavelength / T (m/s) Wave steepness : H / wavelength When H / wavelength = 1/7 or angle at crest 120 or less = Breaker
  • 5. Size of Wind Generated Waves  Depends on 3 things:  Wind Speed  Wind Duration (length of time wind blows)  “Fetch” Extent of open water across which the wind can blow
  • 6. Water Motion in Waves  Water travels in vertical circular orbits  Wave moves, particles don’t!
  • 7. Importance of Waves  Shaping Coastlines  Erode cliffs  Grind rock into sand  Ecology  Returns O2 to water  Stir up food for filter feeders
  • 8. Types of Waves CHOP – Short period (back bays) SWELL – Long period (boat rolls; seasickness) SWASH – water up beach BACKWASH – back down
  • 9. TSUNAMI “TIDAL WAVE” Caused by undersea quake or volcano • Wavelength = ~150 mi. Wave height = 6” – 1’ Can NOT perceive in boat Speed > 500 mph Slows down to ~25 mph at shore; water builds up to ~65+ ft
  • 11. Creation of a Tsunami
  • 12. Tides  The rhythmic rise and fall of the ocean’s water High tide = rising, incoming tide, flow Low tide = receding, outgoing tide, ebb Slack tide = vertical movement stops
  • 13. Tides are very long, slow waves  They have a wave period of 12 hours 25 min  Tidal day is 24 hours 50 min  NJ has 2 high and 2 low tides daily
  • 14. What Causes Tides? 1. Gravitational pull of sun & moon on Earth • Moon closer, therefore > effect • Like magnet, pulls water away from surface = TIDAL BULGE
  • 15. 2. Centrifugal Forces • Bulge on opposite side • Produced by motions of because centr. force > Earth, sun, & moon pull of moon
  • 16. Types of Tides •Spring Tide - Moon and sun are in direct line with one another - Results in unusually high tidal range -Tidal Range = vertical distance between high & low tides  2x’s/month
  • 17. Neap Tide  sun and moon are at right angles  Pulls cancel each other out – causes a weak pull  unusually low tidal range  2 x’s / month
  • 19. Distance bet. Moon & Earth Perigee Tides • Moon closest to earth, very high tides (causes flooding) Apogee Tides • Moon farthest away from earth, very low tides
  • 20.
  • 21. Types of Tides Continued  Diurnal Tides  1 high & 1 low / day  Parts of Gulf of Mexico and Asia  Semi-Diurnal Tides  2 high & 2 low / day  Atlantic coasts of North America and Europe  Mixed  2 high & 2 low / day (height varies)  Pacific coast
  • 22. Importance of Tides • Expose & submerge orgs • Circulate water in bays & estuaries • Circulates food, wastes, etc • Trigger spawning (grunion, horseshoe crab)
  • 23. Currents • What are currents? - “Rivers” of circulating water • Causes - Wind - Rotating Earth - Density Changes
  • 24.
  • 25. Surface Ocean Currents • Broad, slow drifts; never cross equator • Wind generated; circular gyres
  • 26. Coriolis Effect - N. Hemis – clockwise; Right - S. Hemis – counterclockwise; Left
  • 27. • Gulf Stream - N. Atlantic - Brings warm water from equator north along east coast of N. A. -Sometimes form eddies – circulating water that pinches off from the current
  • 28. MIGRATION NAVIGATION WEATHER
  • 29. Localized Surface Currents Longshore Current.  Flows parallel to shore; move sediment
  • 30. RIP CURRENT - Caused by converging longshore currents - Very dangerous ; Red Flag - DO NOT fight rip current; swim parallel to shore to get out of channel
  • 31.
  • 32. Deep Ocean Currents Flow beneath surface; cross equator Move North to South  Separated from surface currents by boundary called a “Thermohaline” (diff in densities)
  • 33. Importance Of Deep  Upwelling Currents • Brings deep water to surf. • Circulates nutrients up • Moves plankton & larvae