Earth Science Final Review Ch. 9-11

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Created by:

mchapman143  on May 13, 2012

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Earth Science

Classes:

Calvary Study Group

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Earth Science Final Review Ch. 9-11

atmosphere
the envelope of the gaseous mixture surrounding Earth
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Terms

Definitions

atmosphere the envelope of the gaseous mixture surrounding Earth
oxygen a colorless, tasteless, odorless, gas that forms approximately 21% of the earth's atmosphere and is the essential element for respiration. It is the most abundant element in the Earth's crust
nitrogen a colorless, odorless, tasteless gas that forms approximately 78% of the earth's atmosphere (by volume)
homosphere one of the zones of the atmosphere when it is subdivided by composition; the layer of the atmosphere nearest the earth's surface consisting of a homogenous mixture of gases
heterosphere one of the zones of the atmosphere defined by composition. It is the collection of gas layers aboce the homosphere consisting of separate layers of oxygen, helium, and hydrogen.
troposphere the lowest of the four layers of the earth's atmosphere defined by the temperature profile. it is the location of all weather that affects the earth's surface.
stratosphere a region of the earth's atmosphere defined by temperature profile located between the troposphere and the mesosphere.
jet stream a high-speed meandering wind current usually flowing from west to east at altitudes of 15 to 25 km. its speed often exceeds 400 km/h.
mesosphere one of the layers of the atmosphere defined by temperature profile. The zone of the earth's atmosphere between about 50-80 km above sea level, characterized by decreasing temperature with increasing altitude.
thermosphere the highest and alrgest of the four atmospheric layers defined by temperature profile, randing from about 80 km-500km above sea level. It is characterized by the highest daily temperatures in the atmosphere.
exosphere the outermost zone of the earth's atmosphere that extends into space itself
ozone layer a layer of concentrated ozone located 20-50km aboce the earth's surface that shields the earth from the harmful forms of ultraviolet light.
ionosphere the portion of earth's upper atmosphere where solar ultraviolet radiation breaks down the gas molecules into individual atoms and ions. It reflects shortwave radio signals. The bottome of the zone starts about 70-80 km about the earth and extends to the edge of the atmosphere.
greenhouse effect the warming off lower atmosphere by infrared radiation that is radiated by the earth's surface after it absorbs visible radiation from the sun.
absolute humidity the amount of water a certain volume of air holds
relative humidity a ration of the amount of water the air is actually holding to the amount it could hold at that same temperature, expressed as a percentage
precipitation moisture falling from the atmosphere as rain, hail, snow, or sleet.
evaporation the process of vaporization when a liquid's temperature is below its boiling point
condensation the change of a gaseous vapor into the liquid state as a result of a decreasing temperature. Occurs in cloud and dew formation.
sublimation a change of state directly from the solid to the gaseous state or from the gaseous state to the solid to the solid state without passing through the liquid state.
freeze the change from the liquid state to the solid state by lowering a liquid's temperature.
melt the change of state from solid to liquid by the application of heat.
dew point the temperature at which air, by cooling becomes saturated with water vapor and the vapor begins to condense around condensation nuclei.
cloud a mass of fine water droplets or ice crystals suspended in the air
Adiabatic cooling cooling of an air mass by a reuction in atmospheric pressure and/or an increase in volume
fog a stratus cloud in contact with the ground
drizzle small slowly falling droplets of rain
dew water that condenses on a cool surface when air in contact with the surface cools to below its dew point
frost the ice crystals that sublimate on a cold surface when a film of air in contact with the surface is cooled to a dew point below freezing
coalescence smaller pieces joining together to form a single larger mass. Raindrops grow in size through this process.
convection the indirect transfer of thermal energy from one place to another by the movement of currents of cooler, more dense matter into regions of warmer, less dense matter. It occurs in liquids and gases because their particles are mobile
orographic the lifting of an air mass and resulting precipitation as it flows over a mountain
front the boundary surface between two dissimilar air masses
frontal wedging vertical movement of a warm air mass due to a wedge of cold air moving under it
freezing rain supercooled water that falls as rain and then freezes on the surface it contacts.

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