1 atmosphere - temp profile wind

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The atmosphere- Page 6

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1 Atmosphere - Temp Profile Wind

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Page 2: 1 Atmosphere - Temp Profile Wind

The atmosphere

• The most significant area of the atmosphere from a meteorological aspect is the Troposphere. It contains 75% of the atmosphere and 90% of the water vapour and is where most of the meteorological activity occurs.

• Various temperature gradients exist in the atmosphere but the most significant is the change at the Tropopause. This area tends to act as a barrier at different heights to the air in the troposphere, which moves in specific ways.

Page 3: 1 Atmosphere - Temp Profile Wind

Composition of the atmosphereGases (invisible) Percentage by volume•Nitrogen 78.09•Oxygen 20.95•Carbon dioxide 00.03•Other constituents – in variable quantities•Water vapour (invisible) – Up to 4% by volume

•Dust particles including clay minerals e.g. kaolinite•Salt particles – Sodium chloride

‘condensation nuclei’

Page 4: 1 Atmosphere - Temp Profile Wind

Atmospheric Pressure

• The surface air pressure at any point will be equal to the density of the air in the column, times the height of the column and gravity.

• The density of the air is controlled by the amount air moving in or out, at the top or bottom of the column.

Page 5: 1 Atmosphere - Temp Profile Wind

Atmospheric Pressure

Force exerted by a column of air on unit area of the earth’s surface.

Units:– hectopascals – hPa, – millibars - mb (1hPa 1 mb)

2

P = ghP – Pressure - mean density of the airg – gravityh – height of the air column

Page 6: 1 Atmosphere - Temp Profile Wind

Atmospheric Pressure

• If the convergence at the troposphere exceeds the divergence at the surface then a high pressure develops at the surface.

• If convergence at the surface exceeds divergence at the troposphere a low pressure develops at the surface.

• The net result from two adjacent areas is a flow of air from the high to the low pressure

Complete diagram

Page 6

Page 7: 1 Atmosphere - Temp Profile Wind
Page 8: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

ght (

km)

TroposphereTropopause

Stratosphere

Page 9: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

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Troposphere

Av ht?__________

TroposphereTropopause

Page 10: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

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km)

Troposphere

Av ht?___12km___

Poles?__________

Equator?________

TroposphereTropopause

Page 11: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

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Troposphere

Av ht?___12km___

Poles?___8-9km__

Equator?_16 km__

TroposphereTropopause

Page 12: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

ght (

km)

Troposphere

Av ht?___12km___

Note – ht of Tropopause is constantly changing

Varies with latitude & season

TroposphereTropopause

Page 13: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

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TroposphereAv T° at Surface?

TroposphereTropopause

Page 14: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

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TroposphereAv T° at Surface? 15°C

Av T° Tropopause

Poles?

Equator?

TroposphereTropopause

Page 15: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

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km)

TroposphereAv T° at Surface? 15°C

Av T° Tropopause

Poles? -60°C

Equator? -80°C

TroposphereTropopause

Page 16: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Heig

ht (k

m)

TroposphereTropopause

Stratosphere

Contains 75% of the total atmospheric mass i.e. gases

Page 17: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

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Troposphere,

Why does T° decrease with height?

TroposphereTropopause

Page 18: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

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Troposphere,

Why does T° decrease with height?

“Warmed from the bottom up”.

Process?

TroposphereTropopause

Page 19: 1 Atmosphere - Temp Profile Wind

• How is the troposphere heated?

Sensible heat (23%)

Latent Heat (77%)

Page 20: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

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Stratosphere

Why does T° increase with height?

TroposphereTropopause

Stratosphere

Page 21: 1 Atmosphere - Temp Profile Wind

Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

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Stratosphere

Why does T° increase with height?

OZONE

Absorbs & filters out UV radiation – leads to warming of strat.

TroposphereTropopause

StratosphereContains OZONE (max)

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Standard Atmosphere - Temperature Profile

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Temperature (deg C)

Hei

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Thermosphere – important 4 life!

Atomic oxygen (O) – absorbs UV radiation – would cause skin cancer

TroposphereTropopause

Stratosphere

Mesosphere

Thermosphere

Page 23: 1 Atmosphere - Temp Profile Wind

Troposphere- Page 7

1. Uniform decrease in temperature with height (10°C - 6.5°C km-1)

2. Wind speed increases with height (no friction).

3. Contains virtually all water vapour (and clouds).

4. Contains “the weather”.5. Contains all major

atmospheric pollution.