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Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christophers Charlie Thomsen

Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

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Page 1: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Chapter 3Atmospheric Energy and

Global Temperatures

Elemental Geosystems 4e

Robert W. ChristophersonCharlie Thomsen

Page 2: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen
Page 3: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Atmospheric Energy and Global Temperatures

Energy Essentials  

Energy at Earth’s Surface  

Temperature Concepts and Controls  

Earth’s Temperature Patterns 

The Urban Environment

Page 4: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Energy Essentials Energy Pathways and Principles 

Shortwave energy in from the Sun

Longwave energy out from Earth

Page 5: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Insolation

Figure 3.2

Page 6: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Energy Pathways

Figure 3.1

Page 7: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Energy PathwaysTransmission

Scattering

Refraction

Albedo and Reflection

Page 8: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Refraction

Figure 3.4

Page 9: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Refraction

Figure 3.3

Page 10: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Albedo and Reflection

Figure 3.5

Page 11: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Clouds and Albedo

Figure 3.6

Page 12: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Heat TransferConduction

Molecule-to-molecule transfer

ConvectionEnergy transferred by movement

AdvectionHorizontally dominant movement

RadiationEnergy traveling through air or space

Page 13: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Heat Transfer

Figure 3.7

Page 14: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Energy Balance in the Troposphere  

The Greenhouse Effect and Atmospheric Warming  

Clouds and Earth’s “Greenhouse”  

Earth–Atmosphere Radiation Balance  

Page 15: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

The Greenhouse Effect and Atmospheric Warming

Atmosphere absorbs heat energy

A real greenhouse traps heat inside

Atmosphere delays transfer of heat from Earth into space

Page 16: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Clouds and Earth’s “Greenhouse”

Figure 3.8

Page 17: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Outgoing Shortwave Energy

Figure 3.9

Page 18: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Outgoing Longwave Energy

Figure 3.9

Page 19: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Earth–Atmosphere Radiation Budget

Figure 3.10

Page 20: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Energy Balance at Earth’s Surface

Daily Radiation Patterns  

Simplified Surface Energy Balance  

The Urban Environment

Page 21: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Daily Radiation Patterns

Figure 3.12

Page 22: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Simplified Surface Energy BalanceNET R =

+ SW (insolation)

– SW (reflection)

+ LW (infrared)

– LW (infrared)

Figure 3.13

Page 23: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Temperature Concepts and ControlsTemperature Scales

Measuring Temperature 

Principal Temperature Controls  

Land–Water Heating Differences

Page 24: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Temperature Scales   

Fahrenheit

Celsius

Kelvin 

Page 25: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Temperature Scales

Figure 3.15

Page 26: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Principal Temperature Controls  Latitude  

Affects insolation

Altitude  High altitude has greater daily rangeHigh altitude has lower annual average

Cloud Cover  High albedoModerate temperatures – cooler days, warmer nights

Page 27: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Effects of Latitude

Figure 3.17

Page 28: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Altitude

Figure 3.18

Page 29: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Land–Water Heating Differences Evaporation

Transparency

Specific heat

Movement

Ocean currents and sea surface temperatures

Marine vs. continental effects

Page 30: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Land–Water Heating Differences  

Figure 3.20

Page 31: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

The GulfStream

Figure 3.21

Page 32: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Marine and Continental Climates

Figure 3.23

Page 33: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Marine and Continental Climates

Figure 3.25

Page 34: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Earth’s Temperature PatternsJanuary Temperature Map  

Thermal equator movement southward

More movement over large continents

July Temperature Map  Thermal equator movement northward

More movement over large continents

Annual Range of TemperaturesContinentality

Page 35: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

January Temperatures

Figure 3.24

Page 36: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

July Temperatures

Figure 3.26

Page 37: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Global Temperature Ranges

Figure 3.28

Page 38: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

The Urban Environment

Figure 3.29

Page 39: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen
Page 40: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen
Page 41: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Urban Heat Island

Figure 3.30

Page 42: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen
Page 43: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Air Temperature and the Human Body

Wind chillCorrelates cold and wind speed

Heat indexCorrelates heat and humidity

Page 44: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Wind Chill Table

Figure 1

Page 45: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

Heat Index Table

Figure 2

Page 46: Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W. Christopherson Charlie Thomsen

End of Chapter 3

Elemental Geosystems 4e

Robert W. ChristophersonCharlie Thomsen