Meteorology Flashcards

1
Q

Typical tropopause heights and temperatures

A

53,000ft (16km) at equator, -75C.
36,000ft (11km) at mid-lat, -56C.
26,000ft (8km) at poles, -45C.

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2
Q

Risk of ground collision when heading to high or low pressure

A

Altimeter will over-read if heading into low pressure risking ground collision.
Think about what would happen if you adjusted to the correct pressure setting (turn down to the lower pressure setting, indicated altitude would fall).

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3
Q

Density altitude
- description
- calc

A

The altitude at which observed air density would be found in an ISA standard atmosphere.
Or, pressure altitude adjusted for ISA temperature difference (@120ft per C)

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4
Q

Depression weather
- Cloud, prec, vis, temp, wind

A

Cloud - extensive (including vertically)
Prec. - Intermittent or continuous, light to heavy
Visibility - Good unless in rain
Temp. - Brings colder air in summer, warmer in winter
Winds - Strong

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5
Q

Anticyclone weather (summer)
- Cloud, prec, vis, temp, wind

A

Cloud - None
Prec. - None
Visibility - Moderate (haze)
Temp - Variable
Wind - Light

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6
Q

Anticyclone weather (winter)
- Cloud, prec, vis, temp, wind

A

Cloud - Low stratus
Prec. - Drizzle
Visibility - Poor (mist/fog likely)
Temp - Warm
Wind - Light

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7
Q

Lifecycle of Atlantic depression

A

4-7 days

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8
Q

Turbulence that pilots should report

A

High level (> FL150) clear air turbulence (i.e. not associated with cumuliform cloud or thunderstorms).
Report time, location, level, intensity and aircraft type

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9
Q

Consequence of temperature error on decision height/altitudes

A

Need to be adjusted when temperature more than 15C below ISA
[increase by 0.4% per deg C]

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10
Q

Jet streams
- position relative to tropopause
- speed
- dimensions

A

Strongest upper thermal winds JUST BELOW tropopause, >60kts (up to 300kts).
Assumed 2000 miles long, 200 miles wide, 2 miles deep. [ratio 1000:100:1]

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11
Q

Jet stream altitudes

A

Equatorial: 50,000ft, 150hPa
Sub-tropical: 40,000ft, 200hPa
Polar front: 30,000ft, 200hPa
Arctic: 20,000ft, 400hPa

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12
Q

Bergeron Theory
(Norwegian or Ice Crystal theory)

A

Bergeron theory is that precipitation is caused by some water droplets turning to ice, growing in size through sublimation with water vapour and colliding with supercooled droplets. These droplets then become heavy and fall as rainfall or snow depending on temp.
Related to the partial pressure of water vapour over ice/water.

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13
Q

Coalescence Theory

A

Assumes a variety of droplet sizes, with larger ones falling faster and uniting with smaller ones, eventually overweight drops fall as DRIZZLE or LIGHT RAIN.

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14
Q

Avoidance distance for thunderstorms on radar (by flight level)

A

0 - FL250: 10NM
FL250-300: 15NM
FL300+: 20NM
Vertical: 5000ft

[Visual avoidance - 10NM]

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15
Q

Thunderstorm risks

A

Turbulence
Hail (up to 45000ft)
Icing (airframe -45 to 0C, carb -10 to 30C)
Lightening (within 5000ft of freezing level, temp -10 to +10C)
Static (affects radio equipment)
Pressure variations
Microbursts
Water ingestion (in jet engine)
Tornadoes

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16
Q

Microburst
- downdraft speed
- windspeed & windshear
- size
- time

A

Down currents in cloud and also outwards due to ground impact.
c. 3000fpm downwards (up to 6000fpm) and 50kt horizontal (in 2 directions, so up to 100kt windshear)
Only 4km horizontal length and last < 5 mins.

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17
Q

Tornado (funnel cloud)
- description
- size
- time

A

Connected to thunderstorms, caused by opposing vertical airflow movements. Diameter generally less than 150m but can be up to 1.6km. Called funnel clouds if they don’t reach the ground (can be embedded within cloud).
Last a few mins up to 30 mins.

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18
Q

Freezing fog

A

With temperatures below 0C air won’t sublime due to lack of freezing nuclei, but will freeze on contact with an object.
Can also happen when fog forms over 0C and air then cools below 0C.

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19
Q

Jet engine icing

A

Jet engines often have some degree of convergence (high air velocity, temp and pressure falls) which can cause intake icing. Operating manual will describe the risk and RPM, airspeed (etc.) to avoid (likely to be high RPM and low airspeed).

20
Q

Polar Front Depressions
- creation
- pressure aloft

A

Main cause of UK bad weather, depressions formed in families along the polar front (mPc, mTw). Warm Tropical air pokes into cold air creating the warm sector. The warm air surrounded by cold will rise and make this a depression.
Move parallel to the warm sector isobars.
Low pressure at high altitude as well as at the ground (unlike warm depressions).

21
Q

Warm front

A

Low slope (1:150) rising over cold air, Ci and stratiform cloud types behind the front.
Total distance of 400/600nm, rain up to 200/300nm under the lower Ns clouds.
Moves at right angles to itself, at 2/3 of the geostrophic interval at the front.

22
Q

Cold front (inc. cloud types

A

Steep slope (1:80) forces warm sector air up quickly, forming Cu, Cb cloud (& Ns) ahead of it - heavy showers. Low pressure at the front itself (so passing of the front sees pressure fall then rise within the cold air following).

23
Q

Passing of warm front
- pressure
- wind direction
- cloud
- precipitation
- temp
- visibility

A

Pressure falls as the centre of the low is approaching you (travelling Eastwards to your north).
Sharp veer from S to SW.
Cloud increases as it approaches (Ci, Cs, As) then Ns and drizzle as it gets closer. Continuous rain as it passes.
Frontal fog as it passes.
Temp & dew point rise as it approaches.
Reducing visibility.

24
Q

Passing of cold front
- pressure
- wind direction
- cloud
- precipitation
- temp
- visibility

A

Pressure low point around the front (closest to centre of the low) then increases after passing.
Sharp veer from SW to NW.
Cu/Cb/Ns cloud, heavy rain or snow showers, thunder/hail possible (air forced upwards steeply by cold front).
Temp & dew point fall.
Visibility good except in showers.

25
Q

Conditions in cold air behind cold front

A

Cumulus clouds (cold air aloft gives steep pressure gradient therefore instability).
Showers
Good visibility

26
Q

Tropical Revolving Storms (TRS)
- Description
- windspeed
- Size
- Time

A

aka hurricanes. Thermal depressions over warm tropical oceans with sustained wind speeds over 33kt. Designated tropical cyclone if sustained wind speed over 63kt [NO LONGER A TRS!, max TRS windspeed 63kt!]
270 NM (500km) diameter
Heavy rainfall
Tornados may be faster, but only last for minutes, TRS last for a couple of weeks.

27
Q

METAR

A

Meteorological Aerodrome Report
Half hourly report of current weather conditions at an aerodrome

28
Q

METAR RVR
- codes

A

“R30/P1500”: RVR > 1500m (i.e. plus)
“R30/M0050”: RVR < 50m (i.e. minus)
If RVR increases by 100m in last 10 mins add “U” at end, if decreases add “D”, if no trend add “N”
Can have two figures separated by “V” if significant variation in last 10 mins.

29
Q

METAR weather codes
“+”
“-“
“ “
“VC”
“=”

A

”+”: Heavy
“-“: Light
“ “: Moderate
“VC”: In the vicinity (within 8km)
“=”: Termination symbol

30
Q

METAR weather codes
“MI”
“BC”
“BL”
“SH”
“TS”
“FZ”
“PR”
“DR”

A

“MI”: Shallow (<2m above ground)
“BC”: Patches
“BL”: Blowing
“SH”: Showers
“TS”: Thunderstorms
“FZ”: Freezing (supercooled)
“PR”: Partial (covering of aerodrome)
“DR”: Drifting

31
Q

METAR precipitation codes
“DZ”
“RA”
“SN”
“IC”
“PL”
“GR”
“GS”
“UP”
“PY”

A

“DZ”: Drizzle
“RA”: Rain
“SN”: Snow
“IC”: Ice Crystals
“PL”: Ice pellets
“GR”: Hail
“GS”: Small hail (<5mm)
“UP”: Unknown precipitation
“PY”: Spray

32
Q

METAR obscuration codes
“BR”
“FG”
“FU”
“VA”
“DU”
“SA”
“HZ”

A

“BR”: Mist (vis 1000 to 5000m)
“FG”: Fog (vis <1000m)
“FU”: Smoke
“VA”: Volcanic Ash
“DU”: Dust
“SA”: Sand
“HZ”: Haze

33
Q

What is obscuration?

A

Something blocking vision that is NOT precipitation (e.g. haze, mist, sand)

34
Q

METAR other codes
“SQ”
“FC”
“SS”

A

“SQ”: Squall
“FC”: Funnel cloud (tornado)
“SS”: Sandstorm/duststorm

35
Q

When is TS included in METAR?

A

Thunder heard in last 10 minutes

36
Q

Cloud types specified in METAR

A

Cb: Cumulonimbus
TCu: Towering Cumulus

37
Q

CAVOK requirements

A
  • Visibility >10km
  • Cloud base >MAX(5000ft, MSA)
  • No Cb or TCu
  • No significant weather in vicinity (e.g. RERA)
38
Q

METAR “RE”

A

“RE”: Recent - in the last hour
e.g. “RETS” thunderstorm in last hour

39
Q

METAR “WS”

A

“WS”: Windshear
Could specify a runway number or “ALL RWY”

40
Q

METAR
“TREND”
“BECMG”
“TEMPO”
“NOSIG”

A

“TREND”: Valid for 2 hours FROM TIME OF OBSERVATION
“BECMG”: Changes becoming permanent
“TEMPO”: Less than one hour and less than half the time period
“NOSIG”: No changes expected in next 2 hours

41
Q

METAR
“SNOCLO”

A

Closed due to contamination

42
Q

METAR components in order (9)

A

EGKK (Location)
121200Z (DDTTTT) [Deduct 1hr for Zulu!]
02015G30KT (Wind)
9999 (Visibility)
R26/0400 (RVR)
DZ (Weather)
FEW020 (Cloud)
18/10 (Temp/DP)
Q1019 (QNH)

43
Q

TAF
“NSC”

A

No significant cloud
Means no cloud below 5000ft or sector altitude, no Cb or TCu, but CAVOK not appropriate.

44
Q

TAF
“TX”
“TN”
“AMD”

A

“TX”: Maximum temperature
“TN”: Minimum temperature
“AMD”: Amendment

45
Q

AIREP

A

Report from pilot on weather (PIREP in USA). Can be handed in at end of flight as written report.
AIREP SPECIAL (or ARS) reported immediately in case of:
Mod/Sev turb or icing
Sev MTW
TS (OBSC, EMBD, WDSPR or SQL)
Heavy dust/sand storm
Volcanic ash

46
Q

Sections of a special AIRREP

A

1) Aircraft identification, position, time, level
2) n/a
3) Meteorological info

47
Q

Where does doppler radar measure turbulence?

A

Thunderstorms, picks up precipitation.