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ES Chapter 23 Leach

ES Chapter 23 The Atmosphere Coach Leach

QuestionAnswer
albedo percent of solar radiation reflected by a surface
atmospheric pressure ratio of the force of the air to the area of the surface on which it presses
barometer instrument that measures atmospheric pressure
climate general weather conditions over many years
conduction type of energy transfer in which vibrating molecules pass heat along to other vibrating molecules by direct contact
convection cell looping pattern of flowing air
doldrums narrow zone of low air pressure at the equator characterized by weak and undependable winds
electromagnetic spectrum complete range of wavelengths of radiation
exosphere layer of the atmosphere above the ionosphere that merges with interplanetary space
greenhouse effect process by which the atmosphere traps infrared rays over the earth's surface
horse latitudes subtropical high-pressure belt of air, around 30 degrees latitude
ionosphere lower region of the thermosphere, at an altitude of 80 to 550 km
jet streams band of high-speed, high-altitude westerly winds
mesopause upper boundary of the mesosphere, marked by an increase in temperature
mesosphere coldest layer of the atmosphere that extends upward from the stratosphere to an altitude of about 80km
nitrogen cycle process in which nitrogen moves from the air to the soil to animals and back to the air
ozone form of atmospheric oxygen that has three atoms per molecule
polar easterlies weak global winds located north of 65 degrees north latitude and south of 65 degrees south latitude that flow away from the poles
standard atmospheric pressure the atmospheric pressure measured at sea level; 760 mm of mercury
stratopause hi-temperature zone that marks the upper boundary of the stratosphere
stratosphere layer of the atmosphere that extends upward from the troposphere to an altitude of 50km; contains most atmospheric ozone
subpolar low belt of low air pressure at about 60 degrees north and 60 degrees south latitude
temperature inversion atmospheric condition in which warm air traps cooler air near the earth's surface
thermosphere the atmospheric layer above the mesosphere
trade winds global winds flowing toward the equator between 30 degrees and 0 degrees latitude
tropopause upper boundary of the troposphere in which the temperature remains almost constant
troposphere atmospheric layer closest to the earth's surface where nearly all weather occurs
weather general condition of the atmosphere at a particular time and place
westerlies global winds located between 40 degrees and 60 degrees latitude that flow from the southwest in the Northern Hemisphere and from the nortwest in the Southern Hemisphere
Created by: CoachLeach
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