air 2 Flashcards
3 important factors determine structure and stability of the atmosphere
gravity of the earth
amount of gas present (DENSITY)
temperature of gases **
temperature changes in atm with
location (amnt of radiation)
Time (season)
altitude
factors that change temperature
orientation of earth w respect to the sun
cloud activity
time of day
volcanic activity
troposphere
turning, changing
unstable
temp decreases w increasing alt
weather occurs here
90% of total mass of atm
tropopause - 10-16km
stratosphere
stratified (layered, ozone)
stable region, particles remain for years
global temperature inversion(warm air (UV absorbed in Ozone) overlies cooler air)
temp increases w alt
9.5% mass of atm
absorbs UV radiation
50 km at stratopause
mesosphere
unstable
temp decreases w alt
.5% mass of atm
shooting stars
85 km st mesopause
lowest lvl of ionosphere
thermosphere
inversion region
air hated by absorbing xrays and other high radiation from sun
highly ionized ionosphere
wind systems driven by
heating by sunlight at earths surface
rotation of earth (coriolis effect)
friction/collision of the atmosphere (slows motion)
(evap and condensation)
hadley cells
move warm air away from tropics - bouyancy
N and S
ferrel cells
moves air from higher latitudes down - subsidence
N and Sj
jet streams
move eat/west
5 major
total global mixing takes
2 yrs