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39 Cards in this Set

  • Front
  • Back
CCNs
hygroscopic: initiate condensation
hydrophobic: retard condensation
ice-forming nuclei freeing nuclei and sublimation nuclei
Radiational Cooling
CLEAR and CALM
NE in Fall
later afternoon Tdew is reasonable estimate of next morning's Tmin
Radiation/Ground Fog
clear night
high humidity at low elevations
light winds
hilly areas
Advection Fog
winter
moist air moves over a cooler surface
warm air to cold ground
Steam Fog (Sea Smoke)
warm water
cold air over water
condensation and fog forms
Cumulus Congestus or TCU
orographic ascent up over green mountains
bubbling appearance
Orographic Towering Cumulus
line of towering cumulus over spine of green mountains
FLAT BASES at lifted condensation level
building clouds are following by rain shafts and virga
Cirrus
HIGH
thing/fine base
angel hair
Cirrocumulus
HIGH
bright
size of thumb
puffy/pure ice
Cirrostratus
halo around sun
bright/looks like sheet
Altostratus
MIDDLE
dim sun
sun looks like pin prick of light
Altocumulus
MIDDLE
fist size
bumpy
darker, larger, lower
Stratus
LOW
closest
not doing anything
pancake
Stratocumulus
LOW
bumps
long flat base
in between cumulus and stratus
Cumulus
LOW
low
puffy
Nimbostratus
ALL HEIGHTS
RAIN OR SNOW PRODUCING
gray and raining all day
Cumulonimbus
ALL HEIGHTS
RAIN OR SNOW PRODUCING
thunderstorms, lightning, hail,
rain for hour and then stop, never all day
Collision-Coalescence
WARM CLOUDS
large droplets fall
attach to smaller droplets
grow then break apart because unstable
bigger now so fall even faster
Bergeron Process
COLD CLOUDS
ice crystal in midst of supercooled liquid water
saturated for liquid, supersaturated for ice crystals
ice crystals grow and water drops shrink
WATER VAPOR PRESSURE transfers water from drops to ice crystal
Rain
snow falls into warm air
Freezing Rain
snow melts, hits cold air, freezes when it hits something

not enough time to refreeze in air
Sleet
Snow melts, refreezes into sleet as it travels through cold air
Snow
Falling into cold air, never melts on way down
Thunderstorm Ingredients and When
1. warm air rising in an unstable environment

2. upper level diverging winds to draw air upwards

WHEN? spring and summer, afternoon and evening
Airmass/Ordinary
SINGLE CELL
develop in warm humid air away from fronts
short lived
rarely produce strong winds and large hail
3 stages: CUMULUS, MATURE, DISSIPATING
downdrafts bring cooling air
Severe
large hail, tornadoes, flash floods
ingredients:
moist unstable air rising
strong vertical wind shear (upper level winds)
long-lasting
supercell and squall line
Squall Line
multi-cell
continuous gust front along leading edge
Super Cell
rotate
long-lived
tends to be separated from other thunderstorms
rain free base
wall cloud - strongest updraft
large hail
mesocyclone
THUNDERSTORMS
Tornadoes - Best Conditions
rotating severe thunderstorms
unstable air
high humidity and dew point
upper level divergence in jet stream
near intense cold fronts and squall lines
Tornadoes - How?
Directional wind shear with height
cyclonic rotation of updraft (mesocyclone)
mesocyclone shrinks horizontally and stretches vertically
increase in speed of spinning air
Hurricanes - Ingredients
over tropical ocean (79 or warmer)
source of latent heat
none poleward of 20 degrees
Hurricanes - How?
light winds
deep layer of very humid air
CONVERGENCE of surface winds
strong Coriolis Force
Hurricane Stages and Eye
1. Tropical Disturbance
2. Tropical Depression
3. Tropical Storm
4. Hurricane

eye: no rain
scattered mid and high clouds
lowest pressure

eye wall: strongest winds, thickest cloud cover, most intense precipitation

smaller the eye, the more intense it is
cP Modification
cold, dense air, stable, moves from source
steam fog forms because crosses warm water
warms, moistens, and becomes unstable
produces precipitation on leeward banks
mP Modification
forms Chinook winds
west to east
modified, dry pacific air leeward side of Rocky
all rained out by time hits east of rockies
Cold Front
TRIANGLES
sharp temperature changes
shift in wind direction and pressure
steep noise
fast moving fronts - squall line with thunderstorms
Warm Front
SEMI CIRCLES
warm, moist air replaces retreating cold air
half the speed of cold air
overrunning: warm air rises over cold - clouds and precipitation ahead of front
Stationary Front
OPPOSING DIRECTIONS OF CIRCLES & TRIANGLES
air flow parallel to the boundary
stalling
associated with FLOODING
Occluded Front
SAME DIRECTION OF CIRCLES & TRIANGLES
cold front catches up and overtakes a warm one
Cold occlusion: colder air behind front
Warm occlusion: milder air behind front