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Chapter 4 APES
| Term | Definition |
|---|---|
| atmospheric convection | Global patterns of air movement that are initiated by the unequal heating of Earth. |
| Hadley cell | A convection current in the atmosphere that cycles between the equator and 30 degrees North and 30 degrees South. |
| Ferrel Cell | A convection current in the atmosphere that lies between Hadley cells and polar cells. |
| Coriolis Effect | The deflection of an objects path due to the rotation of Earth. |
| Rain SHadow | A region with dry conditions found on the leeward side of a mountain range as a result of humid winds from the ocean causing precipitation on the windward side. |
| Polar Cell | A convection current in the atmosphere, formed by air that rises at 60 degrees North and 60 degrees South and sinks at poles 90 degrees North and 90 degrees South. |
| Climate | The average weather that occurs in a given region over a long period of time. |
| Weather | The short term conditions of the atmosphere in a local area, which include temperature, humidity, clouds, precipitation and wind speed. |
| Troposphere | A layer of the atmosphere closest to the surface of Earth, extending up to approximately 16 km. |
| Stratosphere | The layer of the atmosphere above the troposphere, extending roughly 16 to 50 km above the surface of Earth. |
| Angle of Sun rays to Earth | Angle of sun rays are distorted, and solar energy is weaker when it has to pass through Earth's atmosphere on an angle. |
| Albedo | The percentage of incoming sunlight reflected from a surface. |
| Earth's tilt | Earth's tilt causes incoming sunlight to be weaker in the northern hemishpere where it has to pass through more atmosphere. |
| Upwelling | The upward movement of ocean water toward the surface as a result of diverging currents. |
| Thermohaline Circulation | An oceanic circulation pattern that drives the mixing of surface water and deep water. |
| ENSO | El nino; A reversal of the wind and water currents in the South Pacific |