Atmospheric stability & Cloud Formation Flashcards

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
Q

Katabatic drainage shape of graph

A

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
Q

Turbulence inversion graph shape

A

Up to the left. Straight line to the right. Up again the left.

26
Q

Altimeter measures?

A

Measures distance between a/c and sub scale setting