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3000. Environmental lapse rate = 4 °C/km. 2000. Height above the ground ( m). 1000. 0. 0. 5. 10. 15. 20. 25. 30. 35. Temperature ( °C). 3000. Environmental lapse rate = 4 °C/km. 2000. Height above the ground ( m). Dry adiabatic lapse rate. 1000. 0. 0. 5. 10. 15. 20.
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3000 Environmental lapse rate = 4°C/km 2000 Height above the ground (m) 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
3000 Environmental lapse rate = 4°C/km 2000 Height above the ground (m) Dry adiabatic lapse rate 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
3000 2000 Height above the ground (m) 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
3000 2000 Height above the ground (m) 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
3000 2000 Height above the ground (m) 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
Moist adiabatic lapse rate 3000 Environmental lapse rate = 4°C/km 2000 Height above the ground (m) Dry adiabatic lapse rate 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
3000 2000 Height above the ground (m) 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
3000 2000 Height above the ground (m) 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
3000 2000 Height above the ground (m) 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
Absolutely stable 3000 2000 Height above the ground (m) 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
Absolutely stable 3000 warming aloft 2000 Height above the ground (m) and/or cooling near-sfc. 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
Dry adiabatic lapse rate 3000 Moist adiabatic lapse rate Height above the ground (m) 2000 1000 Environmental lapse rate = 11°C/km -5 0 5 10 15 20 25 30 Temperature (°C)
3000 Height above the ground (m) 2000 1000 -5 0 5 10 15 20 25 30 Temperature (°C)
3000 Height above the ground (m) 2000 1000 -5 0 5 10 15 20 25 30 Temperature (°C)
3000 Height above the ground (m) 2000 1000 -5 0 5 10 15 20 25 30 Temperature (°C)
3000 Height above the ground (m) 2000 1000 -5 0 5 10 15 20 25 30 Temperature (°C)
3000 Height above the ground (m) 2000 1000 -5 0 5 10 15 20 25 30 Temperature (°C)
3000 Height above the ground (m) 2000 1000 -5 0 5 10 15 20 25 30 Temperature (°C)
Absolutely unstable Dry adiabatic lapse rate 3000 Moist adiabatic lapse rate Height above the ground (m) 2000 1000 Environmental lapse rate = 11°C/km -5 0 5 10 15 20 25 30 Temperature (°C)
Absolutely unstable 3000 cooling aloft 2000 Height above the ground (m) and/or 1000 warming near-sfc. 0 0 5 10 15 20 25 30 35 Temperature (°C)
Environmental lapse rate = 8°C/km 3000 Moist adiabatic lapse rate 2000 Height above the ground (m) Dry adiabatic lapse rate 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
3000 2000 Height above the ground (m) 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
Conditionally unstable Environmental lapse rate = 8°C/km 3000 Moist adiabatic lapse rate 2000 Height above the ground (m) Dry adiabatic lapse rate 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
Conditionally unstable Dew point 3000 2000 Height above the ground (m) 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
Conditionally unstable Dew point 3000 2000 Height above the ground (m) lifting condensation level 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
Conditionally unstable Dew point 3000 2000 Height above the ground (m) lifting condensation level 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
Conditionally unstable 3000 level of free convection 2000 Height above the ground (m) 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
Conditionally unstable 3000 2000 Height above the ground (m) 1000 0 0 5 10 15 20 25 30 35 Temperature (°C)
620 cal/g 80 cal/g 540 cal/g 80 cal/g 540 cal/g 620 cal/g Fig. 2-2, p.28