AVN 2300: Midterm 2 Mnemonics & Study Craziness
AVN 2300: Last Minute Midterm 2 Mnemonics & Study Craziness
ALL MNEMONICS:
RA = Rain
SN = Snow
SG = Snow Grains
PL = Ice Pellets
GR = Hail
GS = Small Hail or Snow Pellets
DZ = Drizzle
SH = Showers
+ = Heavy
- = Light
FSH: “Friendly Snakes Hide” – Ferrel cell, Subtropical jet stream, Hadley cell
FPP: “Fast Pigs Paint” – Ferrel cell, Polar jet stream, Polar cell
GSMM: “Giant Snakes Make Moves”
G = Global scale
S = Synoptic
M = Meso
M = Micro
“Some silly girls drink good shots, cry good luck”
Some silly girls – Sublimation = solid to gas = ice to water vapor
Drink good shots – Deposition = gas to solid = water vapor to ice
Cry good luck – Condensation = gas to liquid = water vapor to water
Valley Breeze – up mountain slopes (sun heats valley floor).
“Bring valley UPPP!!” – “Bring Sally up!” song
“Saturday Night Live in South Carolina (SC-SN), U DUB (UW-CC) Child Cousins”
SC-SN: Stratus/Nimbostratus = STABLE air = COLD front = CALM weather
long light rain
UW-CC: Cumulonimbus, Cumulus = UNSTABLE air = WARM front = Storms, heavy weather
temps ^, pressure v then ^
Cumulonimbus, Cumulus thunderstorms heavy rain
FOG:
Radiation Fog: Forms overnight in clear, calm conditions due to rapid cooling of the surface (typically in valleys).
Advection Fog: Forms when warm, moist air moves over cooler land or water.
Upslope Fog: Forms as moist air rises up a slope, cooling and condensing to form fog.
Evaporation Fog: Forms when cold air moves over warmer water, causing evaporation and subsequent condensation.
Ice Fog: Forms in extremely cold temperatures, where moisture freezes into ice crystals.
Valley Fog: A type of radiation fog that forms in valleys due to cooling air.
AIRMETS, SIGMETS, CONVECTIVE SIGMETS:
AIRMETs: Moderate hazards (light turbulence, moderate icing, visibility issues)
Below 24,000 feet.
SIGMETs: Severe weather (severe icing, severe turbulence, volcanic ash, dust storms, hurricanes)
Above/Below 24,000 feet. (any altitude)
Convective SIGMETs: Severe thunderstorms, tornadoes, hail, and squall lines, usually affecting altitudes
Below 24,000 feet.
FRONTS:
Cold front: cold overtakes warm, pushes under, steepest front
Abrupt weather changes
Short intense storms/rain
Clear skies follow
Warm front: warm overtakes cold, pushes over, less steep
Overcast, light rain
Warm weather follows
Stationary front: cold and warm meet neither moves much
Gentle slope, can remain for a few days
Occluded front: cold overtakes warm, complex, steep
Heavy rain, clouds, storms
Occlusion = end of storm system
Weather phenomena: “Saturday Night Live in South Carolina (SC-SN), U DUB (UW-CC) Child Cousins”
STABLE AIR = Cold front = CALM weather
temps v, pressure v then ^
Stratus/nimbostratus, long light rain
UNSTABLE AIR = Warm front = Storms, heavy weather
temps ^, pressure v then ^
Cumulonimbus, Cumulus thunderstorms heavy rain
FLIGHT NEAR THUNDERSTORMS:
Dangerous. Because of:
Turbulence, windshear, lightning, hail, icing
Stay 20 nm away or more, alter flight path if necessary, climbing above it if needed is better
Within the storm: updrafts/downdrafts, lightning, thunder, hail, tornadoes = bro watch out
Surrounding the storm: wind shear, squall lines, microbursts, outflow boundaries
What is necessary for the development of microbursts?
Instability, high precipitation water, dry air in the mid levels, and strong winds in dry layer
SCALES:
GSMM = “Giant Snakes Make Moves”
Global scale
Synoptic,
Meso,
Micro
Frontolysis = getting weaker “lys = do break down”
Frontogenesis = birth of a storm “genesis = birth”
HURRICANE STAGES:
Disturbance
Depression
Storm
Hurricane
JET STREAM:
Jet stream: fast flowing ribbon of air
ITCZ: low pressure area near equator
FSH: “Friendly Snakes Hide” – Ferrel cell, Subtropical jet stream, Hadley cell
FPP: “Fast Pigs Paint” – Ferrel cell, Polar jet stream, Polar cell
WINDS:
Daytime: WARM
Sea Breeze – sea to land (land heats up faster)
Valley Breeze – up mountain slopes (sun heats valley floor).
“Bring valley UPPP!!” – “Bring Sally up!” song
Night Time: COLD
Land Breeze – land to sea (land cools faster)
Mountain Breeze – down mountain slopes (cool air sinks).
Katabatic Winds – Cold, dense air rushes downhill (common in polar regions).
Basically just mega extra chilly mountain breezes
Hills & mountains: WARM/HOT
Chinook Winds – Warm, dry winds descending mountains (can rapidly warm areas)
Santa Ana Winds – Hot, dry winds descending in California that fuel wildfires.
TYPES OF AIRMASSES:
c = dry, m = moist
P = cold, T = warm, A = freezing
PRESSURE REMINDERS:
Cold air parcel ^
Warm air parcel v
High pressure v and clockwise
Low pressure ^ and counter clockwise
Converge = goes together
Low pressure (goes up) = converges at the surface
Diverge = goes apart
High pressure (goes down) = diverges at the surface