- Wind is caused by differences in air pressure, which generally occurs due to uneven heating of the atmosphere.
- The two main types of wind are Global Winds, which occur over large areas and Local Winds which occur over relatively smaller areas.
- Winds are generally named after the direction they blow from.”
- Sea Breezes are formed during daytime when the Sun is up and the land is warmer than the sea. This causes a convection current in which the air above the land rises and the cool air over the sea moves in to take it’s place.
- Land Breezes are formed during night time when the Sun is down and the sea is warmer than the land. This causes a convection current in which the air above the sea rises and the cool air over the land moves in to take it’s place.
- A sea breeze blows from the sea and a land breeze blows from the land.
- .Warm air rises from the surface near the Earth’s equator and sinks back to the surface near the poles to create global convection cells.
- These convection cells are disrupted by the Coriolis Effect which is caused by the Earth’s rotation on it’s axis.
- This causes winds in the northern hemisphere to curve to the right and curve to the left in the southern hemisphere.
- The jet stream air currents are found at high altitudes and move 400 km/hour.”
- The polar easterlies are found between the poles & 60 degrees latitude in both hemispheres and travel from east to west.
- The westerlies are found between 30 degrees & 60 degrees latitude in both hemispheres and travel from west to east.
- The trade winds blow from 30 degrees to the equator in both hemispheres.
- Ocean currents are much like wind, but they occur in the worlds oceans.
- Currents are caused when denser water sinks and less dense water rises (another example of convection).
- Water can be denser if it is colder and/or more salty.
- The surface water on the west coast of Europe is warmer because of the North Atlantic Current.
- Examples of how climates can be affected by ocean currents include the west coast of Europe is warmer and wetter than North America at the same latitude.