Atmospheric stability & Cloud Formation Flashcards

(27 cards)

1
Q

Stability is the idea that

A

What goes up must come down. What doesn’t come down, means it’s unstable.

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2
Q

What is the Adiabatic process?

A

Change of pressure, but without heat or matter entering or leaving the system.

Taking into account WATER in air when ISA doesn’t.

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3
Q

Any air that’s below 100% saturation / humidity =

A

Dry air

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4
Q

100% humidity =

A

100% saturated air

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5
Q

DALR (dry air lapse rate) =

A

1⚫️C per 100m

3⚫️C per 1000ft

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6
Q

Saturated air lapse rate (SALR)=

A

1.8⚫️C per 1000ft

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7
Q

Environmental Lapse Rate (ELR) is the…

It is responsible if air is…

A

Actual decrease of temperature with altitude.

  • > ABSOLUTELY UNSTABLE
  • > ABSOLUTELY STABLE
  • > CONDITIONALLY UNSTABLE
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8
Q

Absolutely unstable=

A

Air keeps on going up

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9
Q

Absolutely stable

A

Air falls back down to ground

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10
Q

Conditionally unstable

A

Depends on ELR lapse rate.

-if it’s in between DALR & SALR

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11
Q

If ELR after SALR

A

ELR IS STABLE

nice weather, stratus cloud, small supercooled water droplets, smooth

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12
Q

If ELR before DALR

A

unstable ELR.

= bad weather, fierce clouds, flatline, fluffy cloud, big supercooled water droplets

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13
Q

What is humidity:

A

amount of water vapour in the air.

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14
Q

Saturation

A

The total maximum amount of water vapour that can be held in the air.

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15
Q

What’s used to measure humidity?

A

Tephigram graph or radiosonde

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16
Q

Inversions? Two types

And what do they generally mean?

A

Very stable conditions
Temperatures increase with height
Surface inversion(begins at surface)
Inversion aloft (begins higher in altitude)

17
Q

(Inversion formations)

Surface cooling

A

Ground is cooling. Conducts cool air above it. But there’s warm air higher above, from earlier sunny radiation. (If there’s no strong winds to distort this).

18
Q

Katabatic drainage

A

Cold air moving down into creek, falling below the warm air, (the warm air radiated of the ground of the creek).

19
Q

Frontal inversion

A

Warm air front coming into a envelope of cold air. Warm air can’t quite push the dense cold air, so ends up flowing on top of it.

20
Q

Subsidence inversion

A

Cold air that’s naturally descending compresses up against another cold layer above ground. As these layers are compressed, a higher pressure is formed, resulting in an increase of heat above the surface.
UP TO 6000ft

21
Q

Turbulence inversion

A

As wind rotates, almost barrel rolls, cold air from higher gets pulled down lower and warm air from below gets pushed upwards. UP TO 2000ft

22
Q

Marked Temperature inversions

A
Temp differences 10⚫️c or more
Between surface & 1000ft
warning symbol shown
Affects handling & safety
Marked wind shear at inversion
23
Q

How inversions are cleared:

A

Heating from below
Strong winds
Change of weather pattern

24
Q

Surface cooling graph shape?

What has wind got to be?

A

Graph goes to up to the right. Then goes up to the left.
(X axis temperature(to the right t increases))
(Y axis height (up is gain in height))

24
Katabatic drainage shape of graph
Goes up to the left. Then straight line to the right. Then increases height again to the left. (Temperature on x axis, to the right = positive) (Height on y axis, up on the y axis= increase of height).
25
Turbulence inversion graph shape
Up to the left. Straight line to the right. Up again the left.
26
Altimeter measures?
Measures distance between a/c and sub scale setting