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Unit 6: 8.10 B

Atmospheric Movement

TermDefinition
altitude The vertical distance above sea level
barometer Instrument/tool used to measure air pressure.
global winds The difference in pressure between regions of the Earth creates this. Can influence local weather.
coriolis effect The curving of global winds due to the rotation of the Earth. Creates global circulation cells and wind belts.
hadley cell Located between 0 degrees (equator) to 30 degrees latitude N/S. Winds blow towards the equator from east to west, creating the global wind belt known as the trade wind.
ferrel cell Located between 30 degrees to 60 degrees latitude N/S. Winds blow toward the poles from west to east, creating the westerlies wind belt.
polar cell Located between 60 degrees to 90 degrees latitude N/S. Winds blow away from the poles from east to west, forming the easterlies wind belt.
westerlies Winds blowing toward the poles, west to east, between 30-60 degrees latitude N/S. Responsible for moving weather systems across the US.
easterlies Winds blowing away from the poles, east to west, between 60-90 degrees latitude N/S.
jet streams Global winds that travel in higher altitudes from east to west. There are two jet streams (polar and subtropical) in each hemisphere.
local winds Winds created by mountains, valleys, lakes, and oceans that blow over smaller, shorter distances.
valley breeze A cool wind that blows up a mountain during the day.
mountain breeze a wind that flows down a mountain at night.
monsoon A seasonal change in wind direction caused by differences in heating and cooling of land and water. Can travel farther distances and affect large areas.
high-pressure system Cool, dense air that sinks towards Earth's surface, spinning clockwise. Causes sunny, stable weather conditions.
low-pressure system Warm, less dense air that rises above Earth's surface, spinning counterclockwise. Cause stormy, turbulent weather.
isobars Lines connecting points of equal atmospheric pressure.
meteorologist A scientist who studies weather systems and patterns.
air mass A large body of air that has relatively uniform temperature and humidity. They form when air sits over a region for many days.
cold front Occurs when a cold air mass pushes a warm air mass, forcing the warm air to rise. Showers and thunderstorms can form along the edge of the front.
warm front Occurs when a warm air mass pushes a cold air mass. Produces steady rain along and ahead of the front.
stationary front A boundary between two air masses pushing against each other, neither strong enough to move or replace the other. Mostly forms an overcast sky.
occluded front Forms when two cold air masses cover a warm air mass. Typically forms thunderstorms.
weather map A visual display that shows several forms of weather data. Used by meterologists.
Created by: kmondragon
 

 



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