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

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

Transcript of Chapter 3 Atmospheric Energy and Global Temperatures Elemental Geosystems 4e Robert W....

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

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Atmospheric Energy and Global Temperatures

Energy Essentials  

Energy at Earth’s Surface  

Temperature Concepts and Controls  

Earth’s Temperature Patterns 

The Urban Environment

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Energy Essentials Energy Pathways and Principles 

Shortwave energy in from the Sun

Longwave energy out from Earth

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Insolation

Figure 3.2

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Energy Pathways

Figure 3.1

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Energy PathwaysTransmission

Scattering

Refraction

Albedo and Reflection

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Refraction

Figure 3.4

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Refraction

Figure 3.3

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Albedo and Reflection

Figure 3.5

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Clouds and Albedo

Figure 3.6

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Heat TransferConduction

Molecule-to-molecule transfer

ConvectionEnergy transferred by movement

AdvectionHorizontally dominant movement

RadiationEnergy traveling through air or space

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Heat Transfer

Figure 3.7

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Energy Balance in the Troposphere  

The Greenhouse Effect and Atmospheric Warming  

Clouds and Earth’s “Greenhouse”  

Earth–Atmosphere Radiation Balance  

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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

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Clouds and Earth’s “Greenhouse”

Figure 3.8

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Outgoing Shortwave Energy

Figure 3.9

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Outgoing Longwave Energy

Figure 3.9

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Earth–Atmosphere Radiation Budget

Figure 3.10

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Energy Balance at Earth’s Surface

Daily Radiation Patterns  

Simplified Surface Energy Balance  

The Urban Environment

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Daily Radiation Patterns

Figure 3.12

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Simplified Surface Energy BalanceNET R =

+ SW (insolation)

– SW (reflection)

+ LW (infrared)

– LW (infrared)

Figure 3.13

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Temperature Concepts and ControlsTemperature Scales

Measuring Temperature 

Principal Temperature Controls  

Land–Water Heating Differences

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Temperature Scales   

Fahrenheit

Celsius

Kelvin 

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Temperature Scales

Figure 3.15

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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

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Effects of Latitude

Figure 3.17

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Altitude

Figure 3.18

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Land–Water Heating Differences Evaporation

Transparency

Specific heat

Movement

Ocean currents and sea surface temperatures

Marine vs. continental effects

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Land–Water Heating Differences  

Figure 3.20

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The GulfStream

Figure 3.21

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Marine and Continental Climates

Figure 3.23

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Marine and Continental Climates

Figure 3.25

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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

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January Temperatures

Figure 3.24

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July Temperatures

Figure 3.26

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Global Temperature Ranges

Figure 3.28

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The Urban Environment

Figure 3.29

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Urban Heat Island

Figure 3.30

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Air Temperature and the Human Body

Wind chillCorrelates cold and wind speed

Heat indexCorrelates heat and humidity

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Wind Chill Table

Figure 1

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Heat Index Table

Figure 2

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End of Chapter 3

Elemental Geosystems 4e

Robert W. ChristophersonCharlie Thomsen