weather Flashcards
standard lapse rate
troposphere to 36K’ (temperature constant 36-80K’)
-2°C per 1000’ ↑
-1” pressure (in mercury Hg) per 1000” ↑
inches of mercury at sea level
29.92
where altimeter settings come from
international standard atmosphere
temperature
15C
59F
pressure
14.69 PSI
29.92 in Hg
1013.25 milibar
101.325 kPa
1 atm
density
1.225 kg/m3
anti-cyclonic circulation
because of coriolis effect
using right arm (elbow) as a device to remember
high pressure air moves
clockwise
outward
downward
cyclonic:
low
counter clockwise
inward
upward
use this to predict tailwinds
convective forces
turbulence from:
updrafts at barren places
downdrafts at water or expansive vegetation
turbulence
erratic changes in attitude and/or altitude
eddies and vertical currents
mechanical
lower levels of atmosphere
caused by air experiencing friction due to ground objects
clear air turbulence
most common above ≈15K’
usually jet streams
more in winter
thermal (convective)
uneven heating of earth
frontal
friction 2 opposing air masses
can be severe
commonly associated cold fronts
chop V turbulence
chop = rapid and somewhat rhythmic bumpiness
levels of turbulence
light
momentarily causes slight, erratic changes in altitude and/or attitude (pitch, roll, yaw)
moderate
changes in altitude and/or attitude occur but the aircraft remains in positive control at all times. it usually causes variations in indicated airspeed
severe
causes large abrupt changes in altitude and/or attitude. it usually causes large variations in indicated airspeed. aircraft may be momentarily out of control.
extreme
aircraft is violently tossed about and is practically impossible to control. it may cause structural damage.
reporting turbulence rate
occasional <1/3 time
intermittent 1/3-2/3 time
continuous >2/3 time
wind sheer
sudden drastic change in wind speed or direction over a small area
microburst
most severe wind sheer
parcel of air plummets to ground @ high speed
wet (southeast US) and dry (west US)
1-2 miles
5-15 minutes
loss of 6000’ per minute
can experience headwind loss of 30-90 knots
adiabatic heating and cooling
increasing or decreasing heat through change in pressure (volume compression/expansion)
no heat is actually exchanged
most unstable air
moist warm air
“types” of icing
induction
interferes with engine performance.
in air intake system or farm as carburetor icing. reduces available air available for combustion.
instrument
icing on instruments interfering with data aquisition
structural
*clear - slow freeze along body. most dangerous cause hard to see
*rime - immediate freeze. leading edges
*mixed
-light accumulation over the wings
—reduce lift 30%
—increase drag 40%
-larger accretions
—reduce lift even more (? how much)
—increase drag 80%
-stall at higher air speeds and lower AOA
types of fog
radiation fog
temperature meets dew point overnight as ground temperature drops. more likely if rained previous night. little to no wind needed to occur.
advection fog
needs wind. warm, moist air moves over cold surface. too much wind and will rise to form stratus clouds.
upslope fog
like advection fog. needs wind. blown up hills.
steam fog
cold air moves over warmer water. fog forms from the water. if flown through, icing and low level turbulence can occur.
ice fog
very cold weather (below freezing). evaporating water forms directly into ice crystals. little to no wind needed.
ceiling
SKC - clear
FEW - >0 to 2/8
SCT - scattered - 3/8 to 4/8 clouds
BKN - broken - 5/8 to 7/8 clouds
OVC - overcast 8/8 clouds
CB - cumulonimbus when present
TCU - towering cumulonimbus when present
? what is a cloud
air is cooled and water vapor in atmosphere is saturated and attaches to particles (condensation nuclei). allows vapor to be seen.
cloud types
cumulous
stratus
cloud designations
cirrus - clouds in high atmosphere
alto - clouds in middle of atmosphere
low clouds are combination of stratus, cumulous, and nimbus
nimbus (latin for rain)
types of clouds at AGLs
0-6500’ -
stratus,
stratocumulous,
nimbostratus,
fog
6500’-20K’ -
altostratus (moderate turbulence and icing), altocumulous [altostratus breaking up - usually (light turbulence and icing)]
20K’+ - cirrostratus,
cirrocumulous,
cirrus
other types of clouds
castellanus - look like castles
fracto - looks like braille
lenticularus - over mountains, lens shaped, very strong winds!
most hazardout clouds
towering cumulonimbus because of thunderstorms
for a storm to form
sufficient water vapor
unstable lapse rate (temperature and pressure)
initial uplifting force
phases of thunderstorm
cumulous (developing) phase
-3 to 5 mile height
-lifting action begins
-clouds build in height, moisture, instability
mature phase
-5 to 10 mile height
-rain within about 15 minutes
-both warm air updrafts and cold air downdrafts
dissipating phase
-5 to 7 mile height
-vertical motion slows down
-downdrafts replace previous updrafts
distance to keep from thunderstorms
20 nautical miles
do not fly under or over in little planes
squall line
narrow thunderstorm
usually moist unstable air from cold front but can be separate from any front
turbulence distance from storm
up to 20 miles away
supercooled water
between 0°C and -15°C. freezes on impact with plane