200 likes | 389 Views
Movements of the Ocean. Chapter 21. Ocean Currents. Ocean currents are moving streams of water within the ocean. There are two types of currents: surface currents and deep currents. Surface Currents. Currents that move on or near the surface of the ocean
E N D
Movements of the Ocean Chapter 21
Ocean Currents • Ocean currents are moving streams of water within the ocean. • There are two types of currents: surface currents and deep currents.
Surface Currents • Currents that move on or near the surface of the ocean • 3 factors that control surface currents – air currents, Earth’s rotation, and location of continents • All surface currents are affected by winds
Global Wind Belts • Global wind belts are a major factor affecting the flow of ocean surface water. • Trade winds – located just north & south of equator. Winds blow from northeast in the Northern Hemisphere and blow from southeast in Southern Hemisphere • Westerlies are located in the middle latitudes. Blow from southwest in Northern Hemisphere and from northwest in Southern Hemisphere
Continental Barriers • Continents act as barriers to major surface currents. • When current flows against a continent, the current is deflected & divided. • Coriolis effect = curving path of oceans & winds due to Earth’s rotation • Gyres = wind belts & Coriolis effect cause huge circles of moving water. • Gyres move clockwise in Northern Hemisphere and counterclockwise in the Southern Hemisphere.
Deep Currents • What causes deep currents to move if the wind doesn’t have an effect on it? • Water density moves the water. • Cold water is more dense and it sinks and moves. • Warm water is less dense and it rises. • Note: surface currents travel much faster than deep ocean currents.
What is a Wave? • A wave is a periodic disturbance in a solid, liquid, or gas as energy is transmitted through the medium. • Another kind of wave is described as the periodic up-and-down movement of water. Caused mainly by winds.
Wave Features Wave period = the time it takes 2 consecutive wave crests to pass a given point. A wave’s speed is calculated by dividing wavelength over wave period.
Like the bottle in the diagram, water molecules do not travel horizontally through the water with the wave. Water Movement in a Wave
Since waves receive their energy from wind pushing against the surface of the ocean, then energy received decreases as the depth of the water increases
Wave Size Whitecaps • 3 factors determine the size of the wave • Speed of the wind • Length of time wind blows • Fetch – distance wind can blow across open water • Large waves produced by strong, steady winds blowing across a long fetch. • When wind blows crest of wave off, whitecaps are formed
Undertow – water carried onto a beach by breaking waves pulled back into deeper water by gravity. This motion forms an irregular current. • Rip currents – forms when water from large breakers returns to the ocean through channels that cut through underwater sandbars that are parallel to the beach. • Longshore currents – form when waves approach the beach at an angle.
Tides • Periodic rise and fall of water level in the oceans • High tide – water level is at its highest • Low tide – water level is at its lowest
Cause of Tides • The gravitational pull of the moon on Earth and Earth’s waters is the major cause • Sun also causes tides but they are smaller because the sun is so much farther from Earth than the moon
Tidal range = difference in levels of ocean water at high tide & low tide Spring tides = Occurs during the new moon & full moon; results in higher high tides and lower low tides. Neap tides = occurs during 1st & 3rd quarter moons; daily tidal range is small. Types of Tides