chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 w m 2k 287.05 j kg-i hts...

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Chapter 1

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Page 1: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

Chapter 1

Page 2: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio
Page 3: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

Characteristics of the atmosphere

• Thin film of fluid, under influence of

–Gravity

–Earth’s rotation

–Differential solar heating

Page 4: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio
Page 5: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio
Page 6: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

Characteristics of the

atmosphere

• Density decreases ~exponentially

with altitude

• Falling by a factor e every ~7km

• ~80% of the mass below 10km

Page 7: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

Characteristics of the

atmosphere

• Temperature changes with altitude

–Decreases in the troposphere

• Adiabatic expansion

–Increases in the stratosphere

• Absorption of UV radiation by ozone

Page 8: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio
Page 9: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

• Land covers ~30% of the globe

• NH covers ~70% of total

• Thermal contrasts + topography

Page 10: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio
Page 11: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio
Page 12: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio
Page 13: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

Characteristics of the

atmosphere

• A column of air with the surface density

and ~7-8km thick will excert a pressure

equivalent to 1 atmosphere

Page 14: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

Characteristics of the

atmosphere

• Below ~80km

– The mean free path short and molecular

collisions frequent

– The atmosphere can be regarded as

• a continuum fluid

• in local thermodynamic equilibrium (LTE)

Page 15: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

Dry air

Page 16: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

Dry air

• State variables: p, ρ, T

• Necessary to know only two of them

Page 17: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

• Air is compressible (as opposed to liquids)

Page 18: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

Moist air

Page 19: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio
Page 20: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

Moist air

Page 21: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio
Page 22: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio

• Moisture content decays

rapidly with height

• The tropics more moist

than polar regions

• Clouds form and

precipitation occurs when

moist air is cooled

– Rising air (clouds)

– Radiative cooling (fog)

Moist air

Page 23: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio
Page 24: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio
Page 25: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio
Page 26: Chapter 1 · 1.40 1.293 kg m 105k m s 1.73 x 1.34 x 10 ms 2.40 x 10-2 W m 2K 287.05 J kg-I hts reserved. Specific heat at constant pressure Specific heat at constant volume Ratio