4.5 Global Wind Patterns Flashcards
Convection Cells
Convection cells are circular patterns of air or water movement caused by the uneven heating and cooling of a substance. Hot air or water rises, creating an area of low pressure, while cooler air or water sinks, creating an area of high pressure.
Imagine a pot of boiling soup on a stove. As the heat is applied to the bottom of the pot, the soup near the bottom gets hot and starts rising to the surface. At the same time, as it cools down near the surface, it sinks back towards the bottom. This continuous cycle creates convection cells in your soup!
Polar Cells
Polar cells are atmospheric circulation patterns that occur near the poles. In these cells, cold air sinks and moves towards lower latitudes at surface level, creating a polar high-pressure zone.
Think of a giant ice cream cone with the scoop on top representing the polar region. The cold air sinks down like melting ice cream sliding off the scoop and spreads outwards towards lower latitudes like a chilly breeze.
Ferrel Cells
Ferrel cells are mid-latitude atmospheric circulation patterns located between Hadley cells and polar cells. In these cells, warm air from low latitudes meets cold air from high latitudes, creating a zone of mixing.
Picture two opposing teams playing tug-of-war with different colored ropes. The warm air pulls from one side while the cold air pulls from another side, resulting in a chaotic mix of colors in the middle where they meet.
Hadley Cell
Hadley cells are large-scale atmospheric circulation patterns that occur near the equator. Warm air rises at the equator, moves towards the poles at high altitudes, and then descends back to the surface in subtropical regions.
Imagine a giant conveyor belt moving heat from the equator to the poles and back again. The warm air rises like bubbles in a pot of boiling water, travels along the conveyor belt, and eventually sinks down like cool air settling on a hot stove.
Coriolis Effect
The Coriolis effect is the apparent deflection of moving objects, such as air or water currents, caused by the rotation of the Earth. It causes moving objects to be deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.
Imagine you are on a spinning merry-go-round and you throw a ball towards someone standing at its edge. Instead of reaching them directly, due to your spinning motion, the ball will appear to curve away from them. This is similar to how the Coriolis effect causes moving objects on Earth’s surface to deflect.