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Published byAlicia Skinner Modified over 9 years ago
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the state of the atmosphere at a given time and place depends on: amount of cloudstemperature air pressurewind amount of moisture
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A thick blanket of gases surrounding the Earth composed of AIR (a mixture of gases)
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Nitrogen (N) 78% Oxygen (O)21% Also, Carbon Dioxide (CO 2 ), H 2 O Vapor, and Argon (Ar) in small amounts
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Troposphere: layer of the atmosphere closest to the Earth 10km above the earth where weather happens temperature decreases with height
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3 oxygen atoms bonded together O is an atom of Oxygen (O) O 2 is atmospheric Oxygen (O-O) O 3 is ozone (O-O-O)
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Absorbs 99% of harmful ultraviolet rays from the sun ozone layer is about 10 to 20 km thick thinning is the result of chloroflorocarbons (CFC’s) containing chlorine, fluorine, and carbon
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Stratosphere: second layer of the atmosphere 10-50 km above earth surface where the 90% ozone layer is temperature increases with height where airplanes fly (on edge of troposphere) weather balloons found here
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Mesosphere: third layer of the atmosphere (50-85 km) “meso” means “middle” where meteors burn up (shooting stars) temperature decreases with height
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Thermosphere: outmost layer of the atmosphere (85-500km) As height increases, temperature increases named for its high temp – but you would not feel heat b/c there are so few gas particles due to vacuum (or thin air). thickest layer where auroras happen consists of 2 parts: Ionosphere & Exosphere
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pressure that the air exerts on the Earth directed equally in all directions
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differences in air pressure causes the Earth’s winds and weather changes air pressure is affected by: temperature water vapor elevation
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instrument used to measure air pressure air pressure is reported as: 1.height of mercury column in barometer 2..001 of standard sea level a.p.
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two types: mercury aneroid
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lines that join points on a map having the same air pressure
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falling barometer: warmer weather, humid (rain, snow) rising barometer: cooler weather, drier
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Almost all of the Earth’s energy comes from the sun and is called radiant energy most reaches the atmosphere and is reflected back to space
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Some is absorbed by the Earth and is spread throughout the atmosphere as: Radiation: transfer of energy in form of waves
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conduction: direct transfer of energy from one substance to another Ex. Bare feet on hot sand
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convection: transfer of energy in a fluid air is a fluid- hot air rises, cool air sinks
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As much energy leaves the Earth that comes in ---> Earth’s heat is balanced. greenhouse effect: trapping of the sun’s energy by the Earth
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caused by the burning of fossil fuels- coal, oil, and natural gas- adds CO 2 into air warming effect may melt glaciers and raise sea levels
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Houston on a smoggy day (left) and a clear day (right).
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All winds result from an uneven heating of the atmosphere movement of air two types: (1) local winds
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Flow of cool air from water to land during the day wind
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Flow of cool air from land to water at night wind
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monsoons: major seasonal land and sea breeze most of the year, wind blows from land to sea (dry) part of year, wind blows from sea to land (brings warm, moist air)
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jet stream: narrow belt of strong, high speed air height about 10 to 15 km above N. and S. Hemispheres closely related to weather (2) global winds
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http://www.weatherimages.com/data/imag192.html (current position)
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Coriolis effect: deflection of wind and ocean currents caused by the Earth’s rotation Winds in N. Hemisphere flow to the right Winds in S. Hemisphere flow to the left
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anemometer: instrument that measures wind speed
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wind vane: measures wind direction
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*always points into the wind wind This is an easterly wind because it is blowing from the east
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a measure of the energy in molecules the more energy the molecules have, the hotter it feels
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isotherm: lines on a map that connect places that have the same temperature
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thermometer: instrument that measures temperature alcohol and mercury thermometers used (mercury more accurate)
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water freezes at: 0ºC or 32 ºF water boils at: 100ºC or 212ºF
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