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Tides and Currents




2:55 AM       Author: Tomas U. Ganiron Jr   1
Tides
• are the cyclic rising and falling if Earth’s ocean surface
   caused by the tidal forces of the Moon and the Sun
   acting on the oceans. The changing tide produced at a
   given location is the result of the changing positions of
   the Moon and Sun relative to the Earth coupled with the
   effects of the Earth’s rotation.




2:55 AM               Author: Tomas U. Ganiron Jr              2
Intertidal zone
• Is the strip of seashore that is submerged at
   high tide and exposed at low tide.




2:55 AM            Author: Tomas U. Ganiron Jr    3
A tide is a repeated cycle of sea level changes in the
   following stages:

• Over several hours the water rises or advances up a
  beach in the flood tide.
• The water reaches its highest level and stops at high
  tide. Because tidal currents cease this is also called slack
  water or slack tide. The tide reverses direction and is
  said to be turning.
• The sea level recedes or falls over several hours during
  the ebb tide.
• The level stops falling at low tide. This point is also
  described as slack or turning.

Tides may be semidiurnal (two high tides and two low tides
each day), or diurnal (one tidal cycle per day).

2:55 AM               Author: Tomas U. Ganiron Jr            4
• The various frequencies of astronomical forcing which
    contribute to tidal variations are called constituents.
    Its period is about 12 hours and 24 minutes, exactly half
    a tidal lunar day, the average time separating one lunar
    zenith from the next, and thus the time required for the
    Earth to rotate once relative to the Moon.


• The changing distance of the Moon from the Earth also
    affects tide heights. When the Moon is at perigee the
    range is increased and when it is at apogee the range is
    reduced. Every 7½ lunations, perigee coincides with
    either a new or full moon causing perigean tides with the
    largest tidal range


2:55 AM               Author: Tomas U. Ganiron Jr           5
Current
• A current, in a river or stream, is the flow of
   water influenced by gravity as the water moves
   downhill to reduce its potential energy. The
   current varies spatially as well as temporally
   within the stream, dependent upon the flow
   volume of water, stream gradient, and channel
   geometrics.



2:55 AM            Author: Tomas U. Ganiron Jr      6
Ocean current
• is any more or less continuous, directed movement of
    ocean water that flows in one of the Earth's oceans.
•   Ocean Currents are rivers of hot or cold water within the
    ocean. The currents are generated from the forces
    acting upon the water like the earth's rotation, the wind,
    the temperature and salinity differences and the
    gravitation of the moon.
•   Ocean currents can flow for thousands of kilometers.
    They are very important in determining the climates of
    the continents, especially those regions bordering on the
    ocean.


2:55 AM                Author: Tomas U. Ganiron Jr           7

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Tides and Currents

  • 1. Tides and Currents 2:55 AM Author: Tomas U. Ganiron Jr 1
  • 2. Tides • are the cyclic rising and falling if Earth’s ocean surface caused by the tidal forces of the Moon and the Sun acting on the oceans. The changing tide produced at a given location is the result of the changing positions of the Moon and Sun relative to the Earth coupled with the effects of the Earth’s rotation. 2:55 AM Author: Tomas U. Ganiron Jr 2
  • 3. Intertidal zone • Is the strip of seashore that is submerged at high tide and exposed at low tide. 2:55 AM Author: Tomas U. Ganiron Jr 3
  • 4. A tide is a repeated cycle of sea level changes in the following stages: • Over several hours the water rises or advances up a beach in the flood tide. • The water reaches its highest level and stops at high tide. Because tidal currents cease this is also called slack water or slack tide. The tide reverses direction and is said to be turning. • The sea level recedes or falls over several hours during the ebb tide. • The level stops falling at low tide. This point is also described as slack or turning. Tides may be semidiurnal (two high tides and two low tides each day), or diurnal (one tidal cycle per day). 2:55 AM Author: Tomas U. Ganiron Jr 4
  • 5. • The various frequencies of astronomical forcing which contribute to tidal variations are called constituents. Its period is about 12 hours and 24 minutes, exactly half a tidal lunar day, the average time separating one lunar zenith from the next, and thus the time required for the Earth to rotate once relative to the Moon. • The changing distance of the Moon from the Earth also affects tide heights. When the Moon is at perigee the range is increased and when it is at apogee the range is reduced. Every 7½ lunations, perigee coincides with either a new or full moon causing perigean tides with the largest tidal range 2:55 AM Author: Tomas U. Ganiron Jr 5
  • 6. Current • A current, in a river or stream, is the flow of water influenced by gravity as the water moves downhill to reduce its potential energy. The current varies spatially as well as temporally within the stream, dependent upon the flow volume of water, stream gradient, and channel geometrics. 2:55 AM Author: Tomas U. Ganiron Jr 6
  • 7. Ocean current • is any more or less continuous, directed movement of ocean water that flows in one of the Earth's oceans. • Ocean Currents are rivers of hot or cold water within the ocean. The currents are generated from the forces acting upon the water like the earth's rotation, the wind, the temperature and salinity differences and the gravitation of the moon. • Ocean currents can flow for thousands of kilometers. They are very important in determining the climates of the continents, especially those regions bordering on the ocean. 2:55 AM Author: Tomas U. Ganiron Jr 7