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39 Cards in this Set
- Front
- Back
CCNs
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hygroscopic: initiate condensation
hydrophobic: retard condensation ice-forming nuclei freeing nuclei and sublimation nuclei |
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Radiational Cooling
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CLEAR and CALM
NE in Fall later afternoon Tdew is reasonable estimate of next morning's Tmin |
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Radiation/Ground Fog
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clear night
high humidity at low elevations light winds hilly areas |
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Advection Fog
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winter
moist air moves over a cooler surface warm air to cold ground |
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Steam Fog (Sea Smoke)
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warm water
cold air over water condensation and fog forms |
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Cumulus Congestus or TCU
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orographic ascent up over green mountains
bubbling appearance |
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Orographic Towering Cumulus
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line of towering cumulus over spine of green mountains
FLAT BASES at lifted condensation level building clouds are following by rain shafts and virga |
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Cirrus
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HIGH
thing/fine base angel hair |
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Cirrocumulus
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HIGH
bright size of thumb puffy/pure ice |
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Cirrostratus
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halo around sun
bright/looks like sheet |
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Altostratus
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MIDDLE
dim sun sun looks like pin prick of light |
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Altocumulus
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MIDDLE
fist size bumpy darker, larger, lower |
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Stratus
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LOW
closest not doing anything pancake |
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Stratocumulus
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LOW
bumps long flat base in between cumulus and stratus |
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Cumulus
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LOW
low puffy |
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Nimbostratus
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ALL HEIGHTS
RAIN OR SNOW PRODUCING gray and raining all day |
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Cumulonimbus
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ALL HEIGHTS
RAIN OR SNOW PRODUCING thunderstorms, lightning, hail, rain for hour and then stop, never all day |
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Collision-Coalescence
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WARM CLOUDS
large droplets fall attach to smaller droplets grow then break apart because unstable bigger now so fall even faster |
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Bergeron Process
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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 |
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Rain
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snow falls into warm air
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Freezing Rain
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snow melts, hits cold air, freezes when it hits something
not enough time to refreeze in air |
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Sleet
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Snow melts, refreezes into sleet as it travels through cold air
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Snow
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Falling into cold air, never melts on way down
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Thunderstorm Ingredients and When
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1. warm air rising in an unstable environment
2. upper level diverging winds to draw air upwards WHEN? spring and summer, afternoon and evening |
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Airmass/Ordinary
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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 |
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Severe
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large hail, tornadoes, flash floods
ingredients: moist unstable air rising strong vertical wind shear (upper level winds) long-lasting supercell and squall line |
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Squall Line
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multi-cell
continuous gust front along leading edge |
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Super Cell
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rotate
long-lived tends to be separated from other thunderstorms rain free base wall cloud - strongest updraft large hail mesocyclone THUNDERSTORMS |
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Tornadoes - Best Conditions
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rotating severe thunderstorms
unstable air high humidity and dew point upper level divergence in jet stream near intense cold fronts and squall lines |
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Tornadoes - How?
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Directional wind shear with height
cyclonic rotation of updraft (mesocyclone) mesocyclone shrinks horizontally and stretches vertically increase in speed of spinning air |
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Hurricanes - Ingredients
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over tropical ocean (79 or warmer)
source of latent heat none poleward of 20 degrees |
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Hurricanes - How?
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light winds
deep layer of very humid air CONVERGENCE of surface winds strong Coriolis Force |
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Hurricane Stages and Eye
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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 |
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cP Modification
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cold, dense air, stable, moves from source
steam fog forms because crosses warm water warms, moistens, and becomes unstable produces precipitation on leeward banks |
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mP Modification
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forms Chinook winds
west to east modified, dry pacific air leeward side of Rocky all rained out by time hits east of rockies |
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Cold Front
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TRIANGLES
sharp temperature changes shift in wind direction and pressure steep noise fast moving fronts - squall line with thunderstorms |
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Warm Front
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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 |
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Stationary Front
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OPPOSING DIRECTIONS OF CIRCLES & TRIANGLES
air flow parallel to the boundary stalling associated with FLOODING |
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Occluded Front
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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 |