Aviation weather Flashcards

1
Q

Give some characteristics of high pressure (5)

A

Fairer weather and lighter winds
Moves clockwise around high
Slow moving (couple days)
Air sinks so warming and therefore less chance of hitting dew point
Clear skies so can bring cold weather during winter

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2
Q

Give some characteristics of low pressure

A

Cloudy poor weather with strong winds
Low moves in anticlockwise direction

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3
Q

Thermal low (5)

A

Intense heating overland
Thunderstorms
Land heating quicker than oceans
Happens in summer
Air rising creates low pressure

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4
Q

Polar low

A

Happens in winter
Polar or arctic winds
Gain energy from relatively warm sea compared to relatively low air temp. Struggle to maintain energy over land

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5
Q

Orographic low

A

Where high pressure becomes low pressure on the other side of a mountain. Creates mountain wave and turbulence

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6
Q

Trough

A

Extension of low pressure
Poor weather, clouds, TS, RA, SHRA

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7
Q

At what height are met chart figures given?

A

2000’

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8
Q

Ridge

A

Extension of high pressure.
Similar to high pressure but moves through more quickly (6-18 hours)

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9
Q

Col

A

H
L L
H

Light winds
Variable weather each time one appears
Slow moving

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10
Q

ISA Standards
Pressure -
Temp -
Lapse rate -
Tropopause height and temp -
Sea level density

A

1013.2 hPa
15 degrees c
2deg/1000’
36,090’, -56.5c
1.225kg/m^3

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11
Q

Height of tropopause and what affects its height

A

36090 ISA

Equator - 55,000’. Warmer air, less dense, more volume
UK - 35,000’
Poles - 25,000’

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12
Q

Significance of the tropopause

A

Clouds/weather rarely occur above tropopause
High winds (jetstream) just below tropopause
Clear air turbulence occurs here
Contrails
Engines are more efficient (coldest temperature)

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13
Q

Trigger actions for clouds forming

A

Convection (ground heating)
Orographic uplift (air forced up by high cloud??:??)
Convergence (air pushed up, e.g. during trough)
Mass ascent (fronts)
Turbulence (less common)

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14
Q

Difference between stratus and cumulus

A

Stratus - Flat
Cumulus - Bubbly

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15
Q

What temperature range does most icing occur?

A

0 - -20c

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16
Q

Clear ice

A

Forms in cloud
Just above 0c (medium level)
Large droplets
Freeze slowly, allowing air to escape, therefore dense
Runs back

17
Q

Rime ice

A

Forms in cloud
Higher than clear ice
Small drops
Freezes quickly
Trapped air, less dense
White

18
Q

Which kinds of ice would you experience in cloud

A

Clear and rime ice

19
Q

Hoar frost

A

Forms in clear air
Freezes quickly
Deposition

20
Q

Freezing rain

A

Severe icing
Happens just ahead of warm fronts

21
Q

Severity of icing

A

Trace, pereceptible
Light, 0.5cm, 15-60mins
Moderate, 0.5cm, 15 mins
Severe, 0.5cm, 5 mins

22
Q

METARS

A

Meteorological aerodrome report. Issued every 30 mins. Observations at XX:20 and XX:50

23
Q

Meaning of SPEC B or SPEC M

A

SPEC B - METAR has improved
SPEC M - METAR has deteriorated

Often only stated if new METAR not at regular intervals

24
Q

When will a TAF be ammended?

A

Wind changes by 30 degrees or 10kts
Change of colour state

25
Q

Lapse rates
ISA
DALR
SALR

A

ISA - 2c / 1000’
DALR - 3c / 1000’
SALR - 1.5c / 1000’

26
Q

When does air become ‘saturated’

A

When the temperature and the dew point are the same

27
Q

Fohn affect. What happens on the lee-ward side of the mountain?

A

Warmer
Drier
Higher clouds

28
Q

What is an occluded front?

A

When a cold front catches a warm front

29
Q

^ X ^ X ^

^ . ^ . ^ . ^

A

X means decaying/weakening

. Means strengthening. Air rising and coling creating clouds

30
Q

Cold occlusion
Warm occlusion

A

Cold, the colder low pressure system goes underneath the higher pressure system
Warm, the warmer low pressure system goes over the higher pressure system

31
Q

Frontogenesis
Frontoloysis

A

Frontogenesis - Strengthening front
Frontolysis - Weakening front

32
Q

How is a split front drawn

A

Hollow D or ^