Chapter 8 Climatic Zones and Types

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Chapter 8 Climatic Zones and Types

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Title: Chapter 8 Climatic Zones and Types


1
Chapter 8 Climatic Zones and Types
2
Climate Classification
  • The Purpose of Classifying Climates
  • to understand distribution of climates
  • to compare climates of different places
  • Ancient Greek Classification System

3
Major Climate Groups
  • Tropical Humid Climates (Zone A)
  • Dry Climates (Zone B)
  • Mild Midlatitude Climates (Zone C)
  • Severe Midlatitude Climates (Zone D)
  • Polar Climates (Zone E)
  • Highland Climate (Zone H)

4
Modified Köppen Climate Classification System
5
Köppen Letter Code System
E D C B A B C D E
6
Climate Regions of the World
7
Empirical System
  • Based on
  • Temperature
  • Precipitation
  • Helpful to determine
  • Origins
  • Patterns
  • Change

8
World Distribution of Major Climates
Animation (Seasonal Pressure and
Precipitation Patterns)
  • Three Questions
  • Where are the various climate types located?
  • What are the characteristics of each climate?
  • What are the main dominant controls of these
    climates?

9
Introduction toClimographs(example)
10
Tropical Humid Climates (Zone A)
  • Tropical Wet (Af)
  • Tropical Monsoon (Am)
  • Tropical Savanna (Aw)
  • 15-20 degrees N/S of equator
  • winterless, daily sun
  • warm and moist
  • ITCZ thermal convection/uplift

11
Tropical Wet
12
Tropical Monsoon
13
Monsoonal conditions
14
Tropical Savanna
15
Tropical Savanna and the ITCZ
16
Dry Climates (Zone B)
  • 30 land area
  • dry because lack of uplift
  • deserts lt 10 rain/yr
  • steppes 10-25 rain/yr
  • rainfall is scarce, unreliable and intense
  • Subtropical Desert (BWh)
  • Subtropical Steppe (BSh)
  • Midlatitude Desert (BWk)
  • Midlatitude Steppe (BSk)

17
Influence of Subtropical Highs
18
Subtropical Desert and Steppe
19
Midlatitude Desert and Steppe
20
Mild Midlatitude Climates (Zone C)
  • Mediterranean (Csa and Csb)
  • Humid Subtropical (Cfa and Cwa)
  • Marine West Coast (Cfb and Cfc)
  • 30-60 degrees N/S
  • variable because lack constant heat of tropics
    and continuous cold of polar areas
  • alternating air masses

21
Mediterranean
22
Humid Subtropical
23
Marine West Coast
24
Severe Midlatitude Climates (Zone D)
  • 40-70 degrees N
  • broad temperature range (continentality) long
    cold winter, short summer
  • variable precipitation, more near the coasts
  • Humid Continental (Dfa, Dwa, Dfb and Dwb)
  • Subarctic (Dfc, Dwc, Dfd, Dwd)

25
Humid Continental
26
Subarctic
27
Polar Climates (Zone E)
  • Tundra (ET)
  • Ice Cap (EF)
  • very cold, no significant warming
  • dry, but little evaporation so humid

28
Tundra
29
Ice Cap
30
Highland Climate (Zone H)
31
  • Highland dominant controls
  • Altitude
  • Slope aspect and slope angle
  • Weather variability

32
Global Patterns Idealized
  • General Models of Climate Distribution
  • Idealized seasonal precipitation patterns and
    climates along the west coasts of continents.

33
Climatic Distribution in Africa A Practically
Perfect Example
34
(No Transcript)
35
Global Climate Change
  • Time scale of observations determine what
    patterns of change stand out in the record

36
Global Climate Change
  • Determining Climates of the Past
  • Animation (End of the Last Ice Age)
  • Dendrochronology
  • tree ring samples
  • Oxygen isotope analysis
  • of oceanic sediments
  • Ice cores
  • O O
  • Pollen analysis
  • preservation in crustal
  • materials

18 16
/
ratio
37
Global Climate Change
  • Causes of Long-Term Climate Change
  • Animation (Orbital Variations and
  • Climate Change)
  • Volcanic activity and meteor impacts
  • Fluctuations in orbital output
  • Variations in Earth-Sun relations
  • Greenhouse gas concentrations
  • Feedback mechanisms
  • The roles of the ocean

38
  • Climate Models
  • Global Circulation Models (GCMs)
  • Mathematical models of Earths climate system
  • Computer simulation models of future climates (3)
  • Climate prediction (IPCC)
  • global average temperature increase
  • global warming changes in global climates

39
Global Consequences
  • Climate changes will be observable in our
    lifetime
  • Climates may warm 1 degree F per 25 years (on
    average)
  • Precipitation will increase at higher latitudes
    and decrease at lower latitudes
  • As sea ice melts, sea levels rise
  • More atmospheric/oceanic disturbances
  • hurricanes, tornados
  • heat waves, droughts
  • extremely variable conditions

40
Activity
  • Read Ch. 8
  • In-class
  • Hand out w/ specific climate type(s)
  • Determination of climograph(s)
  • 10 groups, 1 investigation per group
  • Sign-in!
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