OCEAN CURRENTS:

CURRENT: Continuous and directed movement of ocean water

TWO TYPES: Surface Currents Deep Water Currents

SURFACE CURRENTS: 10% of water in ocean The upper 400m of the ocean

DEEP WATER CURRENTS: 90% of water in ocean Waters move around the ocean basins by density differences

Density differences a function of different temperatures and salinity

TWO TYPES OF FORCES: Primary Forces: Start the water moving: Solar Heating Winds Gravity Coriolis Effect

Secondary Forces: Influence where the current goes

SOLAR HEATING: Causes water to expand Water is about 8 cm higher than middle latitudes, thus water wants to flow down slope

WINDS: Winds blowing on surface of the ocean push the water

Water piles up in the direction the wind is blowing

GRAVITY Will pull water “down the hill” when water mounds up

CORIOLIS EFFECT: An inertial effect due to the spinning of the earth

When going towards pole you are coming from an area that is moving faster, thus the deflection with the direction of the Earth’s rotationWhen going to the equator, the deflection goes against the spin of the Earth, due to the spin of the Earth

GYRES: The effect of winds and Coriolis effect results in circular flows of water made of several currents

EKMAN TRANSPORT: Surface water is

blown away by winds, dragging the water beneath it

The deflection due to Coriolis Effect creates a spiral pattern and a net current to the right or left of wind

Results in upwelling

UPWELLING: Nutrient rich water from the deeper parts of the ocean rises to the surface to replace the water blown away

Animation:

DEEP WATER CIRCULATION: Occur where the temperature is cold and relatively high in salinity

Thermohaline Circulation Thermo = heat, haline = salt

EARTH CONVEYOR BELT Salt rich, warm water is blown north by the Gulf Stream, where is cools and sinks

This provides heat to the polar regions and nutrients everywhere

Possibly disrupted by global warming

LOCAL CURRENTS: formed by a combination of tides, winds, waves, and rivers/streams

Longshore currents and rip currents

LONGSHORE CURRENTS: When waves strike the shoreline at an oblique angle, causing resultant waves to move parallel with the shoreline

RIP CURRENTS: Formed when waves push the water in front of it sideways till it can find a path out to sea