Chapter 3 Flashcards
Air
mix of nitrogen, oxygen, small amounts of solid/liquids
Atmospheric density
shallow atmosphere –> more than 50% of atmosphere below Mt Denali elevation
Permanent gases
Nitrogen (78%) and oxygen (21%) argon (1%)
nitrogen = added by decay/burning organic matter + volcanic eruptions, removed by nitrogen fixation + lightning
oxygen produced by vegetation + consumed by organisms
Variable gases
Water Vapor = abundant over warm, moist surfaces; very small amounts over polar regions/deserts –> hence variable; important role in storing latent heat
Carbon dioxide: significant effect on climate (like water vapor), uniform in lower layers of atmosphere, increasing bc of human activities
Ozone = 3 oxygen atoms, located in ozone layer (9-30 miles above Earth), absorbs UV rays
Other = methane, carbon monoxide, sulfur dioxide, nitrogen oxides, many harmful + caused by emissions
Aerosols/particulates
solid/liquid particles small enough to remain suspended in atmosphere
Sources = human activities, volcanic ash, windblown soil
Characteristic’s of aerosols
hygroscopic - many absorb water, so water vapor condenses around “condensation nuclei” –> important for cloud formation
absorb/reflect radiation –> influences temp
Layers of the atmosphere
Troposphere, stratosphere, mesosphere, thermosphere, exosphere
Troposphere (t for turbulent)
1) Depth varies depending on time/place, generally deepest over warm tropics, shallowest over cold poles
Characteristics:
1) temp decreases with increasing altitude (going farther away from heat of surface)
2) tropopause = upper limit of surface-initiated turbulence
3) 80% of atmospheric mass in troposphere
4) most clouds formed here
Stratosphere (s for stagnant)
1) Stagnant air
2) constant temperatures in lower half, after that it increases to max at bottom of Mesosphere
3) ozone layer here
Mesosphere
m for minimum
30 to 50 miles above sea level
temperature reaches minimum, lacks source of warmth, meteors burn up here
thermosphere
1) 50 miles +
2) temperature hot –> UV rays
3) no definite top, merges with exosphere (interplanetary space)
Pressure
Troposphere has most pressure –> most mass
Homosphere
up to 50 miles above sea level
zone of homogenous composition of gases
Heterosphere
Above homosphere –> no homogenous composition of gases
layered by atomic weight –> heaviest at bottom (N2), lightest at top (H)
Ozone layer
O ZONE (2nd)
The silly monkey takes eggs
in lower stratosphere, very small amount of ozone (not that concentrated)