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Earth Science Ch. 15 Review

AB
Altitudethe height of an object above a reference point, such as sea level or the Earth's surface
Air pressurethe measure of the force with which air molecules push on a surface
As altitude increasesair pressure decreases.
tropospherethe lowest layer of the atmosphere and is characterized by a constant drop of temperature with increasing altitude
stratospherethe upper layer of the atmosphere, which lies immediately above the troposphere
mesosphere(literally, the "middle sphere") is the coldest layer of the atmosphere
thermospherethe uppermost layer of the atmosphere, in which temperature increases as altitude increases. The thermosphere includes the ionosphere
Radiationenergy that is transferred as electromagnetic waves, such as visible light and infrared waves
Conductionthe transfer of thermal energy as heat through materials
Convectionthe movement of matter resulting from differences in density that are caused by temperature variations. Convection can result in the transfer of energy as heat.
greenhouse effectthe warming of the surface of the Earth and the lower atmosphere as a result of the buildup of carbon dioxide and water vapor, which absorb and reradiate infrared radiation.
Radiation balancethe balance between incoming energy and outgoing energy.
Global warminga gradual increase in the average global temperatures that is due to a higher concentration of gases such as carbon dioxide in the atmosphere.
Windis created by differences in air pressure. The greater the pressure difference is, the faster the wind moves.
Surface windsgenerally blow from polar, high-pressure areas to equatorial, low-pressure areas
Pressure beltsbands of high or low air pressure that circle the Earth at about every 30° of latitude
convection cella pattern of circulation in which warmer materials rise in one location, while cooler materials sink in another location
Coriolis effectthe curving of the path of a moving object from an otherwise straight path resulting from the Earth's rotation
Trade windsprevailing winds that blow northeast from 30° north latitude to the equator and that blow southeast from 30° south latitude to the equator.
Westerliesprevailing winds that blow from west to east between 30° and 60° latitude in both hemispheres.
Polar easterliesprevailing winds that blow between 60° and 90° latitude in both hemispheres.
Local windswinds that are influenced by the geography of an area.
Acid precipitationprecipitation, such as rain, sleet, or snow, that contains a high concentration of acids, often because of the pollution of the atmosphere
Ozonea gas molecule that is made up of three oxygen atoms
ozone layerthe layer of the atmosphere at an altitude of 15 to 40 km in which ozone absorbs ultraviolet solar radiation.


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Mount Vernon Presbyterian School

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