Ch. 5 : Stability, Cloud Development, Precipiation Flashcards
adiabtic process
if a parcel expands & cools or compresses & warms , with no interchange of heat with uts outside surroundings
as long as the air in parcel is unsaturated (RH <100) the rate of adiabtic cooling or warming is constant
Precipitation
the liquid (or solid) cloud particles may grow in size & fall to surface
dry adiabtic process = 10•C /1000m
if the rising air cools to its dew-point temp, the RH becomes 100% condensation occurs , a cloud forms, and latent heat is released.
moist adiabtic lapse rate= 6•c /1000m
heat added during condensation offsetts some of the cooling due to expansion, the air no longer cools (because latent heat is added to the rising saturated air)
stability (stable air)
condition if paracel is colder than its environmental, it will be more dense, it will want to sink back down to its original level
instability (unstable air)
condition is if paracel is warmer than environment it will continue to rise until reaches same temperature
Envormental lapse rate
rate is the one at which the air temperature surroundings vs how it would be changing if were to climb upward into atmopshere
lapse rate
rate at which the air temperature changes with altitude
condensation level
the elevation above the surface whetr the cloud first forms
conditionally instability
if unsaturated stable air is somehowlifyrd to a level where iy becomes saturated
orographic uplift
forced lifting along topographic barrier ,horizontally moving air, cannot go through obstacle, so the air must go over it
Collison-Coalescence process
large cloud droplets fall faster than small
large droplets collide with smaller droplets
warm cloud
cloud that have above-freezing temperature at all levels
ice-Crystal “Bergeron” process
rain formation proposes that both ice-crystal and liqiud cloud droplets myst co-exist in clouds at temperature belive freezing
super cooled droplets
water droplets exists at temperature below freezing
cold cloud
clouds are able to extend upwards into regions whete air temperature are below freezing
accretion
process of ice crystals growing large as they collide with super cooled cloud droplets
rain
falling drops of liquid water equal to and greater than 0.5 mm
drizzle
smaller than 0.5 mm
virga
evaporating speaks of precipitation
snow
falling precipitation consisting frozen ice crystals or ice crystals clump together to form snowflakes
graupel
considered form of snow heavily rimed snow particles
sleet
upon fallig a snowflake melts fully or pratically , then refreezes into an ice pellet, tend to bounce
freezing rain
rain falls in water liqiud but upon impact on surface as it comes contact with something it freezes due to shallow layer of cold air freezes
hail
large ice precipitation
Droppler Radar
microwave pulse us sent out from the radar transmitter. The pulse strikes raindrops and fraction og its energy is reflected back to do the radar unit, where it is detected and displayed