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Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-132)

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Page 1: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

Surface Energy Balance

Current Weather

Finish Latent Heat

Marine vs. Continental Climates

Surface Energy Balance

For Next Class: Read Chapter 4 (pp. 116-132)

Page 2: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-
Page 3: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

Land–Water Heating Differences  

Figure 5.7

Page 4: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

Marine and Continental Climates:Vancouvervs.Winnipeg

Figure 5.12

Page 5: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

Figure 5.13

Marine and Continental Climates:San Franciscovs.Wichita

Page 6: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

Marine and Continental Climates:Trondheimvs.Verkhoyansk

Figure 5.16

Page 7: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

(b)

(c)

(a)

January Temperatures

Figure 5.14

Page 8: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

8© AMS

Heat Imbalance: Atmosphere vs. Earth’s Surface

Sensible Heating• The Bowen Ratio compares

how heat at the Earth’s surface is divided between sensible heating and latent heating

Varies from one place to another

Depends on amount of surface moisture

Surface energy budget through the course of a year

Page 9: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

Daily Radiation Curves

Figure 4.14

Page 10: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

Surface Energy Budget

Figure 4.15

Page 11: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

Albedo

Figure 4.5

Page 12: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

Simplified Surface Energy Balance

NET R =

+SW (insolation)

–SW (reflection)

+LW (infrared)

–LW (infrared)

Figure 4.16

Page 13: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

Global NET R

Figure 4.17

Page 14: Surface Energy Balance Current Weather Finish Latent Heat Marine vs. Continental Climates Surface Energy Balance For Next Class: Read Chapter 4 (pp. 116-

Radiation Budgets

Figure 4.20

El Mirage, CA

Pitt Meadows,BC