Meteorology Flashcards
(167 cards)
AS (Cloud)
Altostratus
ATIS
- Issue Times
- Heights
- Wind
- Visibility
- Cloud Type
- Issue Times: Irregularly, when conditions change
- Heights: feet AAL
- Wind: Degrees magnetic
- Visibility: 4 digits, in metres for less than 5000m, KM 5000m or more
- Cloud Type: Only if CB or TCU
VA
Volcanic ash
Describe Equatorial Air (Airmass)
Less warm and very moist
Describe the mature stage - Thunderstorms
Due vast amount of water and ice carried aloft, updraughts can no longer provide enough buoyancy and moisture descends, often at high rate. Downdraughts at front portion of the Cb while updraughts continue to function at the rear. Violent turbulence zone is produced between the up and down draughts. As downdraughts hit the surface, they spread out horizontally. Freezing level oscillates, lower in the forward half of the cloud where the downdraughts prevail and higher where the updraughts are found (usually the rear). Onset of downdraughts causes precipitation in the form of heavy showers of water and often more hail. Lasts approx. 15-20 mins.
AMD
Amended
What happens to pressure before, at and after the passage of a cold front?
- Before: Decrease
- At: Arrest of fall
- After: Increase
CAT
clear air turbulence
SA
Sand
GR
Hail (5mm or more)
GS
Small hail (smaller than 5mm)
Warm advection means:
Warm air moving toward colder regions
METAR/METAR AUTO/SPECI
- Issue Times
- Heights
- Area covered
- Wind
- Visibility
- Cloud Type
- Issue Times: METARs on the hour, every hour; AUTOs every half hour
- Heights: feet AAL
- Area: Within 8km of the aerodrome reference point. If term VC is used, it applies between 8 and 16km from aerodrome reference point
- Wind: Degrees True
- Visibility: 4 digits, in metres until 9999m, 2 digits in KM above 9999m (not at AA/WN/CH)
- Cloud Type: Only if CB or TCU
MI
Shallow
Types of thunderstorms
- Orographic Thunderstorms
- Heat type (thermal) thunderstorms
- Convergence Thunderstorms
- Nocturnal equatorial Thunderstorms
- Cold stream (or cold advection) Thunderstorms
- Frontal Thunderstorms

Drizzle
DZ
Drizzle

Hail

Freezing Rain
Difference between gusts and squalls
- Gusts: momentary increases in wind speed. Generally caused by turbulence.
- Squalls: rapid increases in wind speed lasting some minutes then dying away. Caused by weather systems.
What happens to precipitation before, at and after the passage of a warm front?
- Before: Light rain turning to persistent heavy rain
- At: Rain ceases but may change to drizzle
- After: occasional rain or drizzle

Widespread Fog
What happens to pressure before, at and after the passage of a warm front?
- Before: Decrease
- At: Arrest of fall
- After: Steady or slightly rise
Aquaplaning speed formula
Vp=9 x Square root of tyre pressure in psi
























