Meteorology Flashcards

1
Q

Layers of the Atmosphere (T, T, S, S, M, M, T, T, E)

A
Troposphere
Tropopause
Stratosphere
Stratopause
Mesosphere
Mesopause
Thermosphere
Thermopause
Exosphere
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2
Q

Troposphere

A

Lowest layer
Contains most of the water vapour in the atmosphere
Temperature decreases as altitude increases
Majority of weather and clouds occur here

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3
Q

Tropopause

A

Upper boundary layer of the troposphere
The temperature has dropped to about -56C
Jet streams, CAT, thunderstorms

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4
Q

Stratosphere

A

Extends to 160,000’
Temperature increases as altitude increases
Initially, -56 C but gradually rises to 0 C
Strong vertical air motions
Some weather can extend into stratosphere

There is virtually no weather above the stratosphere.

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5
Q

The Standard Atmosphere

A

At sea level:
Air is a perfectly dry gas
Temp 15°C
Standard lapse rate Temp changes 1.98°C per 1000 ft
Pressure 29.92”hg or 1013.25mb at sea level

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6
Q

Pressure - the “Compressibility” of air.

A

Air is not empty space.

It has mass and weight just like any other solid, liquid, or gas.

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7
Q

Density = is mass per unit of volume.

A

affected by temperature.
Warm air molecules move around faster and take up more space.
(warm air is less dense).

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8
Q

The Barometer

A

The more force applied to the surface of the mercury in the bowl, the higher the mercury rises in the tube.

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9
Q

Units of Measurement
A pressure decrease or increase equals 1 inch of mercury per 1000’.
Ex:

A

01.00 = 1000’

29.92 Hg is standard pressure for sea level (ISA).
If the pressure were to rise or fall 1 “Hg, the result would be:
30.92 = -1000’
28.92 = +1000

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10
Q

Station Pressure

A

The actual weight of air (pressure), at the station.

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11
Q

Sea Level Pressure

A

The pressure calculated down to mean sea level pressure; or, the station pressure plus the weight of the air extending from the station to mean sea level

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12
Q

City A is at sea level with pressure of 29.92 Hg

–City B is at 5000’ MSL what is their Hg?

A

5,000 = 5.0 Therefore 29.92 -5.0 = 24.92.

Remember when higher in the air (+5,000ft) = less pressure = take away from the mercury reading.

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13
Q

Density Altitude

A

is pressure altitude corrected for temperature.
“Density altitude is the altitude the airplane feels it is at.”
–airplane will be most vulnerable to a high density altitude during takeoff.

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14
Q

Pressure Systems

A

govern the evolution of fronts and weather.

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15
Q

Low Pressure Systems

A
  • -aka: depression or cyclone.
  • -Winds converge at surface = upward motion
  • -Winds flow counterclockwise and toward a low.
  • -weather associated with a low is always bad however the temperature becomes more stable
  • -may cover anything from a very small localized area to half a continent.
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16
Q

High Pressure Systems

A

aka: anti-cyclone.
- -Winds blow clockwise and away from a high
- -Winds converge at altitude = descend then diverge at the surface.
- -Weather is usually fair and clear.

17
Q

Convergence and Divergence

A

–always flow away from highs and towards lows.

18
Q

Isobars

A

These are lines of equal pressure depicted on a pressure map

  • these lines circle areas of pressure and never cross
  • separated by 4 millibars (another word for hpa) intervals
19
Q

Ridge

A

A ridge is an elongated area of high pressure

–Fine to fair weather can be expected.

20
Q

Trough

A

A trough is an elongated area of low pressure.

Poor frontal weather can be expected.

21
Q

Col

A

A col is an area of neutral pressure.

Weather can be unpredictable.

22
Q

Wind and Pressure Gradient

[pressure gradient = rate of change of pressure over a given distance]

A
  • -Isobars spaced closely together indicate rapid change of pressure = Expect strong winds.
  • -Isobars spaced further apart indicate slow change of pressure = Expect light winds
23
Q

Coriolis Force

A

air is influenced by earth’s rotation.
doesn’t flow in straight lines
–high to a low. It is deflected to the right (north)
–deflected to the left in southern hemisphere
Deflection is more pronounced at the poles and zero at equator.

24
Q

Buy-Ballot’s Law

A

northern hemisphere, winds blow

  • -counterclockwise around low pressure (cyclone)
  • -clockwise around a high (anticyclone).

stand with your back to the wind, the low pressure will always be on your left.

25
Q

Surface Friction

A

The reduction of wind speed decreases the Coriolis effect, causing wind to flow outward from a high, and inward to a low.

26
Q

Veer

A

A wind change in a clockwise direction

In a climb, wind usually veers and increases.

26
Q

Back

A

A wind change in a counter-clockwise direction.

In a descent, wind usually backs and decreases.

27
Q

Gusts

A

A rapid irregular fluctuation in the upward and downward movement of air currents.

28
Q

Squalls

A

A sudden and sustained increase in the strength of wind lasting longer than a gust.

29
Q

Land Breezes

A

winds blow from land –> sea
at night
when the land is cooler than the water.

30
Q

Sea Breezes

A

winds blow from sea –> land
during the day
when the water is cooler.

31
Q

Valley Breezes

A

These anabatic winds flows up the slope of a valley during the day, when the air on the sun-facing side becomes warmer and rises.

32
Q

Mountain Breeze

A

These katabatic winds flow down the slope of a valley at night as the air is cooled and is pulled down the slope by gravity.

33
Q

Mountain Wave

A

air flows over a ridgeline it also flows down the other side = oscillations or waves to occur.

  • -can last for several hours
  • -can reach up to 30 nm past the mountain range.
34
Q

Mountain Wave Clouds (3 types)

A

1) Cap Cloud - Forms along top of ridge and the wind carries it downstream.
2) Lenticular - Lens shaped clouds that form along the crest of wave.
3) Rotor Clouds - Form in eddies downstream about ridge height.

35
Q

Wind Shear

A

A distinct change in wind speed and/or direction.

36
Q

Types of wind sheer (2)

A

1) Performance Increasing Shear
Increased head wind
Airspeed increased, aircraft comes in high, overshoots runway
2) Performance Decreasing Shear
Decreased head wind
Airspeed decreases, potential stall at low altitude, undershoots runway