GEOG110 Exam 2 Flashcards
name the 5 fog types
advection radiation (ground/morning fog) upslope (valley fog) frontal autumn-steam
what fog type involves cold air moving over a warm surface
autumn-steam
how is fog formed in the 4 popular fog types
by warm air moving over a cool surface and raising relative humidity
name the 3 types of convection processes
strong heating at earth’s surface
forced convection
slantwise convection
strong heating at earth’s surface
upward moving air that forms cumulus clouds
forced convection
air uplift caused by orography, coastlines, or large urban areas
slantwise convection
occurs along fronts
why are adiabatic processes possible?
air is a poor conductor of heat
what are the 3 types of ELR?
normal - decrease in temp with increase height
inverted - increase in temp with increase height
isotherm - temps remains same with height
what rate does temp normally decrease at
-.8 C / 100m or -8 C / 1km
what are the 2 adiabatic lapse rates
dry (unsaturated) RH
what is the condensation level
the level where clouds form
dry ALR
-1 C / 100 m
wet ALR
-.6 C / 100m
why is dry ALR a conserved quantity and why is WLR not?
the rate is the same weather rising or falling when dry
when wet a heat source is required to raise the air through evaporation (this heat source lowers the W-ALR)
what type of weather does sinking air indicate
fair weather and a stable atmosphere
what type of weather does rising air indicate
thunderstorms and unstable atmosphere
what does it mean when the ELR = ALR
neutral atmosphere (rare)
what is the level of free convection?
where the air in parcel is warmer than ELR and continues to rise
creates an unstable atmosphere and cumuloforms
what kinds of clouds are stable?
startiform
sensible heating and where?
heat gained or lost due to temp changes across surfaces (deserts)
latent heating and where?
heat gained or loss due to phase change of water (jungles)
latent heat and energy taken from environment
evaporation
latent heat and energy released into environment
condensation
why is there relative humidity
the air can hold different levels of moisture depending on the temperature
dew point
temperature of condesation