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The Atmosphere

AB
ozonea gas formed by the addition of a third oxygen atom to an oxygen molecule
tropospherethe layer closest to Earth's surface
stratospherea layer of the atmosphere made primarily of concentrated ozone
mesospherethe third highest layer of the atmosphere from Earth's surface where temperature decreases as elevation increases
thermospherethe fourth layer of the atmosphere that contains only a minute portion of the atmosphere's mass
exospherethe outermost layer of Earth's atmosphere that contains helium and hydrogen
radationthe transfer of energy through space by visible light
conductionthe transfer of energy that occurs when molecules collide through contact
convectionthe transfer of energy by the flow of a heated substance
temperaturea measurement of how rapidly or slowly molecules move around
heatthe transfer of energy that occurs because of a difference in temperature between substances
dew pointthe temperature to which air must be cooled at constant pressure to reach saturation
condensationwhen matter changes state from a gas to a liquid
lifted condensation levelthe height at which condensation occurs
temperature inversionan increase in temperature with height in an atmospheric layer
humiditythe amount of water vapor in air
relative humiditythe ratio of water vapor in a volume of air relative to how much water vapor that volume of air is capable or holding
condensation nucleismall particles in the atmosphere around which cloud droplets can form
orographic liftingthe method of cloud formation
stabilitythe ability of an air mass to resist rising
latent heatstored energy
coalescencewhen cloud droplets collide and join together to form a larger droplet
precipitationincludes all forms of water, both liquid and solid, that fall from clouds
water cyclethe constant movement of water between the atmosphere and Earth's surface
evaporationthe process of water changing from a liquid to a gas


G. Gier

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