Meteo Flashcards
Supercool water
-40c
Tropopause
Not vary altitude, not continue
Dewpoint associated with
temp and relative humidity
Earth
Stratosphere
Icing condition
0 to -5c (ตอบอันที่ร้อนสุด)
Thermal depend on
เกิดจาก Solar heat
Metar
Runway visual range
บินแบบ cross country เข้า headwind
Best lift/drag(L/D), decrease a/s
In northern hemisphere airmass move by
Colioris
Cool, dense air lift warm air
Pressure gradient force
Approaching Thunderstorm with hail
Several mile downwind from under Thunderstorm
Northern hemisphere
High-clockwise, low-counter clockwise
Radiation fog
Calm night
Observer visibility during landing under IFR called
RVR(runway visual range)
ISOBAR
Equal pressure
Equator
Temperature higher than polar
Temp of tropopause
Warm than either side
When cool air replace warm
Convection
8000’ (top cumulus cloud at 8000’ greatest turbulence will expect at)
5000’
lapse rate 4c/1000’
The air is absolute stable
Sea level under standard condition
1013mb 59F 15c 29.92in.hg.
Condition when soaring vicinity Thunderstorm
wind shear and turbulence
Thunderstorm most hazard aircraft
Squall line Thunderstorm
fog become stratus cloud
heat from industrial area
why front hazardous flight
front spoils… …decrease lift
the formation of radiation fog
warm, moist … flatland … clear calm night
cloud with greatest turbulence
Cumulonimbus
a sudden increase wind speed 15 knots/1min
Squall
frost
temperature … adjacent below freezing
CAV-OK
when all of these condition exist
ice pellet at surface is evidence
a temperature inversion with freezing rain at higher altitude
wind shear occur
at any altitude, sudden variation in wind speed or direction
cycle of TS, predominately by downdrafts
Dissipating
flying across front is a change in
wind direction
frost affect a/c t/o
frost may prevent … airborne … normal t/o speed
cloud associated with warm front
all form of start with rain and fog
temp, dew point, spread small, decrease 62F
Fog or low clouds
the area of strongest turbulence encountered when departing a jet stream
Below the core on the polar side
Convection circulation + seabreeze cause by
Cool dense air moving inland from over the water