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Major Ocean Currents
 An Ocean Current is a
large volume of water
flowing through the
ocean.
 Types of Currents:
Surface Currents Caused by Wind Warmer Currents
Deep Currents
Caused by Density
Differences
Colder Currents
Surface Currents
 Surface currents extend to
about 400 m below the
surface, and they move as fast
as 100 km/day.
 Earth’s major wind belts
influence the formation of
ocean currents and the
direction they move.
 Surface Current Patterns
 East Coast – warm current
 West Coast – cold current
Surface Currents Animation
 http://www.classzone.com/books/earth_science/terc/
content/visualizations/es2401/es2401page01.cfm
Coriolis Effect
• Earth’s rotation
makes the wind
curve, as a result,
the ocean’s surface
currents curve.
Coriolis
Effect
Curve to the LEFT in
the SOUTHERN
HEMISPHERE.
Curve to the RIGHT
in the NORTHERN
HEMISPHERE.
 Currents form small or
large loops and move
at different speeds,
depending on the land
masses they contact.
Effects on Climate
 Warm-water currents
and cold-water currents
affect weather and
climate in different
ways
 Regions near warm-
water currents are often
warmer and wetter than
regions near cold-water
currents
Effects on Climate
 The Gulf Stream is a warm-water current that affects
coastal areas of the southwestern United States by
transferring lots of thermal energy and moisture to the
surrounding air.
 The cold California
Current affects
coastal areas of the
southwestern United
States.
Effects on Climate
 https://www.youtube.com/
watch?v=zAGr4Mfbg-E
Effects on Climate
 Examine the link and animation below:
 http://www.classzone.com/books/earth_science/terc/
content/investigations/es2403/es2403page01.cfm?cha
pter_no=investigation
Upwelling
Upwelling is movement of
cold water upward from the
deep ocean often occurring
along coastlines.
1. Wind blows across the ocean’s surface
2. Water is pushed water away from an area.
3. Deeper colder water then rises to replace it,
bringing cold, nutrient-rich water from
deep in the ocean to the ocean’s surface.
Upwelling animation
 http://www.classzone.com/books/earth_science/terc/
content/visualizations/es2405/es2405page01.cfm?chap
ter_no=visualization
 Examples of Upwelling – El Nino/La Nina:
http://www.classzone.com/books/earth_science/terc/
content/visualizations/es2405/es2405page01.cfm?chap
ter_no=visualization
Deep Density-Salinity Currents
 Density Currents are a type of vertical current that
carries water from the surface to deeper parts of the
ocean.
 Density Currents are
caused by changes in
density rather than
wind (SALINITY)
 Density currents
circulate thermal
energy, nutrients and
gases throughout the
world.
Deep Water Density Currents
Great Ocean Conveyor Belt
 The Great Ocean conveyor Belt is the name for a model of
the large system of ocean currents that affects weather and
climate by circulating thermal energy around Earth.
 In this model, high salinity water cools and sinks in the
North Atlantic, and deep water returns to the surface in the
Indian and Pacific Oceans through upwelling
Great Ocean Conveyor Belt
 Scientists estimate that the Great Ocean Conveyor Belt
model takes about 1,000 years to complete a cycle.

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Climate and Ocean Currents

  • 1.
  • 2. Major Ocean Currents  An Ocean Current is a large volume of water flowing through the ocean.  Types of Currents: Surface Currents Caused by Wind Warmer Currents Deep Currents Caused by Density Differences Colder Currents
  • 3.
  • 4. Surface Currents  Surface currents extend to about 400 m below the surface, and they move as fast as 100 km/day.  Earth’s major wind belts influence the formation of ocean currents and the direction they move.  Surface Current Patterns  East Coast – warm current  West Coast – cold current
  • 5. Surface Currents Animation  http://www.classzone.com/books/earth_science/terc/ content/visualizations/es2401/es2401page01.cfm
  • 6.
  • 7. Coriolis Effect • Earth’s rotation makes the wind curve, as a result, the ocean’s surface currents curve. Coriolis Effect Curve to the LEFT in the SOUTHERN HEMISPHERE. Curve to the RIGHT in the NORTHERN HEMISPHERE.  Currents form small or large loops and move at different speeds, depending on the land masses they contact.
  • 8.
  • 9. Effects on Climate  Warm-water currents and cold-water currents affect weather and climate in different ways  Regions near warm- water currents are often warmer and wetter than regions near cold-water currents
  • 10. Effects on Climate  The Gulf Stream is a warm-water current that affects coastal areas of the southwestern United States by transferring lots of thermal energy and moisture to the surrounding air.  The cold California Current affects coastal areas of the southwestern United States.
  • 11. Effects on Climate  https://www.youtube.com/ watch?v=zAGr4Mfbg-E
  • 12. Effects on Climate  Examine the link and animation below:  http://www.classzone.com/books/earth_science/terc/ content/investigations/es2403/es2403page01.cfm?cha pter_no=investigation
  • 13.
  • 14.
  • 15.
  • 16.
  • 17. Upwelling Upwelling is movement of cold water upward from the deep ocean often occurring along coastlines. 1. Wind blows across the ocean’s surface 2. Water is pushed water away from an area. 3. Deeper colder water then rises to replace it, bringing cold, nutrient-rich water from deep in the ocean to the ocean’s surface.
  • 18.
  • 19. Upwelling animation  http://www.classzone.com/books/earth_science/terc/ content/visualizations/es2405/es2405page01.cfm?chap ter_no=visualization  Examples of Upwelling – El Nino/La Nina: http://www.classzone.com/books/earth_science/terc/ content/visualizations/es2405/es2405page01.cfm?chap ter_no=visualization
  • 20.
  • 21. Deep Density-Salinity Currents  Density Currents are a type of vertical current that carries water from the surface to deeper parts of the ocean.  Density Currents are caused by changes in density rather than wind (SALINITY)  Density currents circulate thermal energy, nutrients and gases throughout the world.
  • 22. Deep Water Density Currents
  • 23. Great Ocean Conveyor Belt  The Great Ocean conveyor Belt is the name for a model of the large system of ocean currents that affects weather and climate by circulating thermal energy around Earth.  In this model, high salinity water cools and sinks in the North Atlantic, and deep water returns to the surface in the Indian and Pacific Oceans through upwelling
  • 24.
  • 25. Great Ocean Conveyor Belt  Scientists estimate that the Great Ocean Conveyor Belt model takes about 1,000 years to complete a cycle.