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TIDES
Presented by:
M Sajjad
Roll # 907
BS(Hons) 5th
Geography
PH# 03346544625
CONTENTS
•   Introduction
     •   Definition
     •   Theories
           •   The Equilibrium Theory of Tides
           •   The Dynamic Theory of Tides
•   Tides are generated by…
•   Types of tides
     •   Neep tides
     •   Spring tides
     •   Proxigean Spring Tide
•   Interesting facts
•   Tidal Energy
•   References
INTRODUCTION
• The Greek navigator and
  explorer Pytheas       first
  wrote the connection
  between the position of the
  moon and height of tides
  (399B.C.), But a full
  understanding of tides had
  to await Newton’s analysis
  of gravitation.
DEFINITION


     “periodic rise and fall of all ocean waters, including
   those of open sea, gulfs, and bays, resulting from the
   gravitational attraction of the moon and the sun upon
             the water and upon the earth itself.”

    (Microsoft ® Encarta ® Encyclopedia 2005 © 1993-2004 Microsoft Corporation. All rights reserved.)
EQUILIBRIUM THEORY
• The equilibrium theory of tides explains many characteristics of
  ocean tides by examining the balance and effects of the forces
  that allow a planet to stay in a stable orbit around the sun, or the
  moon to orbit earth.
• The equilibrium theory assumes that the seafloor does not
  influence the tides and that the ocean conforms instantly to the
  forces that affect the position of its surface.
• The ocean surface is presumed always to be in equilibrium
  (balance) with the forces acting on it.
DYNAMIC THEORY OF TIDES
• The dynamic theory of tides, first proposed in 1775 by Laplace,
  added a fundamental understanding of the problems of fluid
  motion to Newton's breakthrough in celestial mechanics.
• The dynamic theory explains the differences between predictions
  based on Newton's model and the observed behaviors of tides.
TIDES ARE GENERATED BY…
Gravitational pull of the moon and sun


                                   Centripetal force of the rotating Earth
TYPES OF TIDES

Neep tides
•During the moon's quarter phases the sun and moon work at right angles, causing the
bulges to cancel each other. The result is a smaller difference between high and low tides
and is known as a neap tide.


Spring tides
•   When the moon is full or new, the gravitational pull of the moon and sun are combined. At
    these times, the high tides are very high and the low tides are very low. This is known as
    a spring high tide
The Proxigean Spring Tide

•This is a rare, unusually high tide. This very high tide occurs when the moon is both unusually
close to the Earth (at its closest perigee, called the proxigee) and in the New Moon phase (when
the Moon is between the Sun and the Earth). The proxigean spring tide occurs at most once
every 1.5 years.
INTERESTING FACTS
• Spring tides and neap tide levels are about 20% higher or lower than
  average.
• The highest tides in the world are at the Bay of Fundy in Nova Scotia,
  Canada.
• The type of gravitational force that causes tides is know as "Tractive"
  force.
• The sun's gravity also produces tides. But since the forces are
  smaller, as compared to the moon, the effects are greatly decreased.
•   Moon has 2x greater gravitational pull than the sun
•   Sun is 10 million x more massive than the moon and is 390 times
    farther away
TIDAL ENERGY
• The energy of tides has been harnessed to produce electricity. In
  the summer of 1966, a tidal power plant with a capacity of 240,000
  kw went into operation on the Rance River, an estuary of the
  English Channel in northwestern France.
(Microsoft ® Encarta ® Encyclopedia 2005 © 1993-2004 Microsoft Corporation. All rights reserved)
GLOBAL DISTRIBUTION
REFERENCES

• Microsoft ® Encarta ® Encyclopedia 2005 © 1993-2004 Microsoft
  Corporation. All rights reserved
Retrieved from
•   http://www.physicalgeography.net/fundamentals/8r.html
•   http://geography.about.com/od/physicalgeography/a/tides.htm
•   http://home.hiwaay.net/~krcool/Astro/moon/moontides/
•   http://www.opportunityenergy.org/?p=316
                                                                  (14-01-2012)
QUESTIONS &
SUGGESTIONS……
THANKS FOR
YOUR PATIENCE

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Tides

  • 1. TIDES Presented by: M Sajjad Roll # 907 BS(Hons) 5th Geography PH# 03346544625
  • 2. CONTENTS • Introduction • Definition • Theories • The Equilibrium Theory of Tides • The Dynamic Theory of Tides • Tides are generated by… • Types of tides • Neep tides • Spring tides • Proxigean Spring Tide • Interesting facts • Tidal Energy • References
  • 3. INTRODUCTION • The Greek navigator and explorer Pytheas first wrote the connection between the position of the moon and height of tides (399B.C.), But a full understanding of tides had to await Newton’s analysis of gravitation.
  • 4. DEFINITION “periodic rise and fall of all ocean waters, including those of open sea, gulfs, and bays, resulting from the gravitational attraction of the moon and the sun upon the water and upon the earth itself.” (Microsoft ® Encarta ® Encyclopedia 2005 © 1993-2004 Microsoft Corporation. All rights reserved.)
  • 5. EQUILIBRIUM THEORY • The equilibrium theory of tides explains many characteristics of ocean tides by examining the balance and effects of the forces that allow a planet to stay in a stable orbit around the sun, or the moon to orbit earth. • The equilibrium theory assumes that the seafloor does not influence the tides and that the ocean conforms instantly to the forces that affect the position of its surface. • The ocean surface is presumed always to be in equilibrium (balance) with the forces acting on it.
  • 6. DYNAMIC THEORY OF TIDES • The dynamic theory of tides, first proposed in 1775 by Laplace, added a fundamental understanding of the problems of fluid motion to Newton's breakthrough in celestial mechanics. • The dynamic theory explains the differences between predictions based on Newton's model and the observed behaviors of tides.
  • 7. TIDES ARE GENERATED BY… Gravitational pull of the moon and sun Centripetal force of the rotating Earth
  • 8. TYPES OF TIDES Neep tides •During the moon's quarter phases the sun and moon work at right angles, causing the bulges to cancel each other. The result is a smaller difference between high and low tides and is known as a neap tide. Spring tides • When the moon is full or new, the gravitational pull of the moon and sun are combined. At these times, the high tides are very high and the low tides are very low. This is known as a spring high tide
  • 9.
  • 10.
  • 11. The Proxigean Spring Tide •This is a rare, unusually high tide. This very high tide occurs when the moon is both unusually close to the Earth (at its closest perigee, called the proxigee) and in the New Moon phase (when the Moon is between the Sun and the Earth). The proxigean spring tide occurs at most once every 1.5 years.
  • 12. INTERESTING FACTS • Spring tides and neap tide levels are about 20% higher or lower than average. • The highest tides in the world are at the Bay of Fundy in Nova Scotia, Canada. • The type of gravitational force that causes tides is know as "Tractive" force. • The sun's gravity also produces tides. But since the forces are smaller, as compared to the moon, the effects are greatly decreased. • Moon has 2x greater gravitational pull than the sun • Sun is 10 million x more massive than the moon and is 390 times farther away
  • 13.
  • 14. TIDAL ENERGY • The energy of tides has been harnessed to produce electricity. In the summer of 1966, a tidal power plant with a capacity of 240,000 kw went into operation on the Rance River, an estuary of the English Channel in northwestern France. (Microsoft ® Encarta ® Encyclopedia 2005 © 1993-2004 Microsoft Corporation. All rights reserved)
  • 16.
  • 17. REFERENCES • Microsoft ® Encarta ® Encyclopedia 2005 © 1993-2004 Microsoft Corporation. All rights reserved Retrieved from • http://www.physicalgeography.net/fundamentals/8r.html • http://geography.about.com/od/physicalgeography/a/tides.htm • http://home.hiwaay.net/~krcool/Astro/moon/moontides/ • http://www.opportunityenergy.org/?p=316 (14-01-2012)