Lesson 4- Ocean Currents
Ocean Currents Overview
Ocean currents: Broad bands of ocean water that flow in specific directions and connect different geographical locations.
Purpose and Role of Ocean Currents
Heat transportation: Carries heat across the Earth, regulating temperatures.
Climate influence: Affects regional climates and weather patterns.
Biodiversity transport: Moves marine creatures globally, impacting ecosystem dynamics.
Types of Ocean Currents
A) Horizontal Currents
Also known as surface currents.
Location: Flow through the top 100-200 meters of ocean water.
Driving forces: Primarily driven by winds.
Influencers of direction:
Uneven heating of the atmosphere: Creates pressure differences leading to wind generation.
Earth's rotation: Causes the Coriolis effect.
Continents: Deflects currents when encountered.
B) Vertical Currents
Definition: Currents that flow beneath the surface, including upward and downward movements.
Types:
Density currents: Result from density differences caused by temperature and salinity variations.
Thermohaline currents: Driven by differences in water density influenced by temperature (thermo) and salinity (haline).
Factors Influencing Ocean Currents
1. Uneven Heating of the Atmosphere
Mechanism: Warm air rises, producing low pressure, while cool air moves in, generating winds.
2. Rotation of the Earth
Coriolis Effect:
Causes currents in the Northern Hemisphere to bend to the right (clockwise).
Southern Hemisphere currents bend to the left (counterclockwise).
Influence of trade winds and westerlies on equatorial and polar currents.
3. Continents
Deflection: Currents turn when they hit continental landmasses, influencing their flow direction.
Formation of Gyres: The combined effects of wind, Coriolis, and continental deflection create circulation patterns in gyres.
Gyres
Definition: Large systems of rotating ocean currents caused by the Coriolis effect.
Major Gyres:
North Atlantic Gyre
South Atlantic Gyre
Indian Ocean Gyre
North Pacific Gyre
South Pacific Gyre
Thermohaline Circulation
Global Conveyor Belt: Refers to the cycle of thermohaline currents driven by density differences in ocean water.
Mechanism of the Conveyor Belt
Begins as cold, dense water sinks near the poles, creating currents that flow towards warmer regions.
Components:
Cold, dense water moves to the ocean floor.
Warm water rises to the surface as currents travel upwards along landmasses.
Upwelling
Definition: A process where deep, cold water rises to the surface.
Occurrence: Common in coastal areas due to offshore winds.
Ecological impact: Enriches surface water with nutrients, supporting marine life and local fisheries.
Importance of Upwellings
Feed major fishing industries, especially along coastal regions like the U.S. West Coast and Peru.