Atmosphere PPT Flashcards
why is the atmosphere important?
contains gases crucial for life, protects the earth from meteorite impact, blankets the earth and traps heat to create a temperature comfortable for life, protects the earth from dangerous rays from the sun
atmosphere
a gaseous layer that surrounds the planet or other celestial bodies
primary atmosphere
existed during earth’s formation, lost early in earth’s history by solar wind
secondary atmosphere
result of volcanic degassing, earth began to cool down, oxygen was finally introduced
air
gaseous envelope surrounding earth, composed of 78% nitrogen and 21% oxygen and trace amounts of other gases found in earth’s atmosphere, invisible
trace gases
absorb certain wavelength of the sun, act as warming blanket of the earth, shield the earth against deadly ultraviolet radiation
variable components of air
water vapor and aerosols
aerosols
liquid droplets or solid particles that are so small that they remain suspended in the air (ex: water droplets in fog, smoke particles from fire, sea salt crystals from ocean spray, volcanic products), can block sun’s radiation
sources of global aerosol sources
dust, volcanic products (SO2), smoke, salt from sea spray
solar radiation is both ___ and ___
absorbed by atmosphere, ocean, land, and biosphere (70%) and reflected back by the outer atmosphere (30%)
characteristics of layers in the atmosphere
different types and proportions of gases, density of gas, temperature changes within the layers, source of energy/heat
list the layers of the atmosphere
troposphere, stratosphere, mesosphere, thermosphere
troposphere
contains 80% of the mass of the atmosphere, most heat-absorbing gases (green house gasses), 0-15 km, all weather occurs here, airplanes
stratosphere
contains 19% of the atmosphere’s total mass, contains the ozone layer where ozone is concentrated, absorbs uv and heat, 15-50 km
mesosphere
temperature decreases with height, 50-80 km, meteors burn up here
thermosphere
temperature increases with height, 80-160 km, international space station satellite orbits the earth
ozone layer
located in the stratosphere, absorbs UV radiation, protects earth’s surface life, basically a shield against radiation
ozone depletion
CFCs breaking down ozone
CFC
cholorofluorocarbons, chemicals commonly used as refrigerants, propellants (in sprays), and solvents, have created a recurring ozone hole
greenhouse effect
process through which long-wavelength (infrared) heat energy is absorbed by gases in the atmosphere, absorption of energy warms earth’s surface
greenhouse effect step by step
- earth’s surface absorbs short-wavelength solar radiation and becomes warmer
- earth’s surface re-radiate the energy as long-wavelength radiation
- molecules of certain gases in the atmosphere absorb some of the heat, and the atmosphere becomes warmer
greenhouse gases
CO2, water vapor, methane
sources of CO2, methane, nitrous oxide, and fluorinated gases
CO2 - fossil fuel
methan - agricultural activities and waste management
nitrous oxide - agricultural activities and fertilizer
fluorinated gases - industrial processes, refrigeration
atmospheric pressure
pressure exerted by earth’s atmosphere because of the weight of overlying air, air pressure decreases with increasing altitude, unit = bars and millibars
measuring device for atmospheric pressure
barometer
wind
horizontal motion of air, caused by differences in atmospheric pressure, air moves from high to low pressure (which creates convection loops), occurs in response to a pressure gradient
pressure differences are caused by…
unequal heating in the atmosphere; hot air rises (low pressure on the ground) and cool air sinks (high pressure on the ground)
coriolis effect
caused by the Earth’s rotation, deflect winds
deflect wind towards…
right for northern hemisphere, left in the southern hemisphere
tornados
violent windstorms produced by a spiraling column of air that extends downward from a cloud, generally peak in May and move from SW to NE
hurricanes
warm sea water, have a coriolis force, low-level disturbance, weak vertical wind shear