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MOVEMENTS OF OCEAN
WATER
K.SUGUNA.R
PGT GEO
THREE TYPES OF MOVEMENTS
• WAVES

• TIDES

OCEAN CURRENTS
WAVES
•
•
•

HORIZONTAL MOVEMENT OF WATER TOWARDS THE COAST
AND AWAY FROM THE COAST
CAUSED BY WIND
WHEN THE WIND MOVES OVER THE WATER SURFACE,IT
MAKES THE WATER PARTICLES TO MOVE
CHARACTERISTICS OF WAVES
•
•
•

WAVE HEIGHT:VERTICAL DISTANCE BETWEEN TOP OF THE
CREST AND THE BOTTOM OF TROUGH
WAVE LENGTH: HORIZONTAL DISTANCE BETWEEN THE TWO
SUCCESSIVE CRESTS
WAVE PERIOD:TIME INTERVAL BETWEEN TWO SUCCESSIVE
WAVES TO TOUCH A FIXED POINT.
TIDES
• THE PERIODICAL RISE AN FALL OF THE SEA LEVEL
• ONCE OR TWICE A DAY
• DUE TO THE ATTRACTION OF THE SUN AND THE
MOON.
SURGE
• MOVEMENT OF WATER BY
METEOROLOGICAL
EFFECTS(CYCLONE)
TYPES OF TIDES
• SPRING TIDES:
•
•
•

RISE VERY HIGH AND FALL VERY LOW
NEW MOON DAYS AND FULL MOON DAYS
SUN ,MOON AND EARTH ARE IN STRAIGHT LINE

• NEAP TIDES
•
•
•

NEITHER RISE VERY HIGH NOR FALL VERY LOW
QUARTER MOON DAYS
SUN ,MOON AND EARTH ARE IN RIGHT ANGLE
OCEAN CURRENTS
• LIKE RIVER FLOW IN OCEANS
• FLOW OF REGULAR VOLUME OF
WATER IN A DEFINITE PATH AND
DIRECTION
TYPES OF OCEAN CURRENTS
•
•
•
•
•
•
•
•

WARM CURRENT:
MOVES FROM HOT REGION TO CCOLD REGION
MOVES ALONG THE SURFACE OF THE OCEAN
INCREASES THE TEMPERATURE OF THE REGION ALONG WITH IT FLOWS
COLD CURRENT
MOVES FROM HOT REGION TO CCOLD REGION
MOVES ALONG THE SURFACE OF THE OCEAN
INCREASES THE TEMPERATURE OF THE REGION ALONG WITH IT FLOWS
TYPES OF OCEAN CURRENTS
•
•
•
•
•
•
•
•

WARM CURRENT:
MOVES FROM HOT REGION TO CCOLD REGION
MOVES ALONG THE SURFACE OF THE OCEAN
INCREASES THE TEMPERATURE OF THE REGION ALONG WITH IT FLOWS
COLD CURRENT
MOVES FROM HOT REGION TO CCOLD REGION
MOVES ALONG THE SURFACE OF THE OCEAN
INCREASES THE TEMPERATURE OF THE REGION ALONG WITH IT FLOWS

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Movements of ocean water

  • 2. THREE TYPES OF MOVEMENTS • WAVES • TIDES OCEAN CURRENTS
  • 3. WAVES • • • HORIZONTAL MOVEMENT OF WATER TOWARDS THE COAST AND AWAY FROM THE COAST CAUSED BY WIND WHEN THE WIND MOVES OVER THE WATER SURFACE,IT MAKES THE WATER PARTICLES TO MOVE
  • 4. CHARACTERISTICS OF WAVES • • • WAVE HEIGHT:VERTICAL DISTANCE BETWEEN TOP OF THE CREST AND THE BOTTOM OF TROUGH WAVE LENGTH: HORIZONTAL DISTANCE BETWEEN THE TWO SUCCESSIVE CRESTS WAVE PERIOD:TIME INTERVAL BETWEEN TWO SUCCESSIVE WAVES TO TOUCH A FIXED POINT.
  • 5. TIDES • THE PERIODICAL RISE AN FALL OF THE SEA LEVEL • ONCE OR TWICE A DAY • DUE TO THE ATTRACTION OF THE SUN AND THE MOON.
  • 6. SURGE • MOVEMENT OF WATER BY METEOROLOGICAL EFFECTS(CYCLONE)
  • 7. TYPES OF TIDES • SPRING TIDES: • • • RISE VERY HIGH AND FALL VERY LOW NEW MOON DAYS AND FULL MOON DAYS SUN ,MOON AND EARTH ARE IN STRAIGHT LINE • NEAP TIDES • • • NEITHER RISE VERY HIGH NOR FALL VERY LOW QUARTER MOON DAYS SUN ,MOON AND EARTH ARE IN RIGHT ANGLE
  • 8. OCEAN CURRENTS • LIKE RIVER FLOW IN OCEANS • FLOW OF REGULAR VOLUME OF WATER IN A DEFINITE PATH AND DIRECTION
  • 9. TYPES OF OCEAN CURRENTS • • • • • • • • WARM CURRENT: MOVES FROM HOT REGION TO CCOLD REGION MOVES ALONG THE SURFACE OF THE OCEAN INCREASES THE TEMPERATURE OF THE REGION ALONG WITH IT FLOWS COLD CURRENT MOVES FROM HOT REGION TO CCOLD REGION MOVES ALONG THE SURFACE OF THE OCEAN INCREASES THE TEMPERATURE OF THE REGION ALONG WITH IT FLOWS
  • 10. TYPES OF OCEAN CURRENTS • • • • • • • • WARM CURRENT: MOVES FROM HOT REGION TO CCOLD REGION MOVES ALONG THE SURFACE OF THE OCEAN INCREASES THE TEMPERATURE OF THE REGION ALONG WITH IT FLOWS COLD CURRENT MOVES FROM HOT REGION TO CCOLD REGION MOVES ALONG THE SURFACE OF THE OCEAN INCREASES THE TEMPERATURE OF THE REGION ALONG WITH IT FLOWS