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Climates and Climate Classification
Climate
• Climate is weather over time
• Climatology is the study of climate
• Climatic regions are areas with similar weather statistics
Earth’s Climate System and Its Classification
• Climate Components
• Classification of Climatic Regions
• A Climate Classification System
Climate Components
• Insolation
• Temperature
• Pressure
• Air Masses
• Precipitation
Earth’s Climate System
Climate Classification -- Two Approaches
• Empiric– Classes are based on observations and the
effects of the phenomena– Examples include Koeppen and Thornthwaite
• Genetic– Classes are based on causes of the
phenomena– Examples include Air-Mass, Synoptic
Classifications, etc.
The Elements of Climate
• Based on– Temperature– Precipitation– Pressure– Wind Direction/Speed– Cloud Cover– “Climate proxies”
Climographs
The Koeppen System
• The Major Climates– The Tree Climates
• A - Tropical Rainy Climates• C - Midlatitude Rainy Climates (mild winter)• D - Midlatitude Rainy Climates (cold winter)
– Trees Don’t Grow Here• B - Dry Climates• E - Polar Climates
Generalized Climate Regions
Figure 6.4
Koeppen System: Principal Climate Types
• Tropical– Af - Tropical Wet (Rains all year)– AW - Tropical Wet/Dry (Dry Winter Season)– Am - Tropical Monsoon (Shorter Dry Season)
• Dry– BW - Desert (BWh - hot desert, BWk, cold desert)– BS - Steppe (semi-arid) BSh - hot steppe, BSk, cold steppe)
• Mesothermal– Cfa, Cwa - Humid Subtropical– Csa, Csb - Mediterranean– Cfb, Cfc - Marine West Coast
Koeppen System: Principal Climate Types
• Microthermal– Dfa, Dfb Dwa, Dwb - Humid Continental– Dfc, Dwc, Dfd, Dwd - Subarctic
• Polar– ET - Tundra– EF - Ice Cap (Remember, Eternally Frozen!)
• Highland Climates
Koeppen System: The Particulars
• First Letter - – Designates Major Type (A, B, C, D, E)
• Second Letter– If with A, C, or D climates, denotes seasonality of
precipitation (f - all year, w=dry winter, s=dry summer)– If with B, denotes whether hot (h) or cold (k)
• Third Letter – Designates different temperature regimes and
sometimes other parameters like fog frequency, etc.
The Factors Forming the Koeppen System
Figure 6.5
Tropical Climates
Tropical Climates
• ~ 12 hours a day throughout the year
• There is a greater daily energy change than there is annual energy change
• Influenced by the migration of the ITCZ
• No temperature constraints on growth leading to large species diversities
Figure 4.11
Movement of the ITCZ
Tropical Rain Forest(Tropical Wet)
(Af)
Figure 6.6
Tropical Monsoon(Am)
Figure 6.7
Figure 6.8
Tropical Savanna(Tropical Wet-Dry)
(AW)
Dry, Arid, and Semiarid Climates
• Desert Characteristics
• Low-Latitude Hot Desert Climates
• Midlatitude Cold Desert Climates
• Low-Latitude Hot Steppe Climates
• Midlatitude Cold Steppe Climates
Dry, Arid, and Semiarid Climates
Low-Latitude Hot Desert(BWh)
Figure 6.21
Low-Latitude Hot Steppe(BSh)
Figure 6.23
Midlatitude Cold Desert(BWk)Figure 6.22
Midlatitude Cold Steppe
Figure 6.24
Mesothermal Climates
• Humid Subtropical – Hot, Humid Summer
• Marine West Coast – Mild All Year, No Dry Season
• Mediterranean – Dry Summer
Mesothermal Climates
Figure 6.9
Humid Subtropical Hot-Summer
(Cfa)
Figure 6.11
Marine West Coast(Cfb, Cfc)
Figure 6.12
Marine West Coast(Cfc)
Mediterranean Climates(Csa, Csb)
Figure 6.14
Microthermal Climates
• Humid Continental Hot-Summer Climates
• Humid Continental Mild-Summer Climates
• Subarctic Climates
Microthermal Climates
Humid Continental Hot-Summer (Dfa, Dwa)
Humid Continental Mild-Summer (Dfb, Dwb)
Figure 6.16
Subarctic (Dfc, Dwc)
Figure 6.17
Subarctic (Dfd, Dwd)
Figure 6.18
Polar Climates (ET, EF)
• Tundra Climate
• Ice Cap and Ice Sheet Climates– Polar Marine Climate
Polar and Highland Climates
Hypothetical Climate Model
http://www.colorado.edu/geography/class_homepages/geog_1001_s06/HypoContinent.pdf
Reality
Climate Classification – The Genetic Approach
• Based on what causes climates, not based on categories determined by observations
• For example….
General Atmospheric Circulation and Climate Regimes
Figure 4.13
TropicalAridTransitionalPolar
Genetic Classification Scheme:An Air-Mass Dominance Example
Wet All Year Wet /Dry Dry All Year
Warm
Seasonal
Cold
1
7
4 5 6
2 3
98
Equatorial Low
Subpolar Low
Subtropical High
Polar High
mT
mP cP
cT
Climates and Water Resource Issues
Robert W. ChristophersonCharlie Thomsen
“When the well is dry, we know the worth of water…”
- Benjamin Franklin
Water Resources– Soil - Water budget concept– Water availability– Soil moisture availability
Ocean and Freshwater Distribution
Figure 5.3
Hydrologic Cycle Model - Revisited
Figure 7.1
The Hydrologic Cycle• A Hydrologic Cycle
Model – More Evaporation over
Oceans than over Land– More Precipitation over
land than over oceans– Amount of water
advected to the land equals the amount runoff back to the oceans
• Surface Water – Only .333% of all surface
fresh water is available for human use.
– 11.20% of all fresh water is available for human use in groundwater and soil moisture
The Soil-Water Balance Equation
Figure 7.2
Surface-Moisture Environment
Figure 7.2
Remember…
• If the air rises, it’s more likely to rain (or snow…)• Where it sinks, it’s less likely to rain (or snow…)
• The less rainfall you have…– The less reliable it is
• So, a climate with a dry season, isn’t necessarily guaranteed a wet season either!– Monsoon climates– Steppe and Savannah Climates– Deserts (obviously)
Precipitation in North America
Figure 7.4
Potential Evapotranspiration
Figure 7.6
Lysimeter
Figure 7.5
Types of Soil Moisture
Figure 7.7
Sample Water Budget
Figure 7.9
Sample Water Budgets
Figure 7.10
Annual Global River Runoff
Figure 7 .11
Groundwater Resources
• Groundwater Profile and Movement
• Groundwater Utilization
• Pollution of Groundwater Resources
Groundwater Potential
Figure 7.12
Groundwater Characteristics
Figure 7.13
Groundwater Characteristics
Figure 7.13
High Plains Aquifer Overdraft
Figure 1
Our Water Supply
• Water Supply in the United States
• Instream, Nonconsumptive, and Consumptive Uses
• Future Considerations
U.S. Water Budget
Figure 7.17
1. Three-fourths of what falls is evaporated
2. We withdraw and consume one-third of what is left on a one-time basis
3. Some of the water is exchanged into groundwater which might not be recoverable
Water Withdrawal by Sector
Figure 7.18
Global Water Scarcity
Figure 7.19
Future Considerations• There’s plenty of water (if you like salt with your water!)
and we don’t loose any of it…
• On a local basis, water resource scarcity is a very real issue
• Too much water and the water becomes polluted
• Too little water and the water becomes polluted
• Water scarcity globally are major issues where:1. The water is used mostly for agriculture and thus for growing the
food supply and…
2. Where competing regions are sharing the same water supply
Global Climate Change
• Global Warming
• Climate Models and Future Temperatures
• Consequences of Global Warming
• Political Action to Slow Global Warming
Global Temperatures
Figure 6.25
1998 Temperature Anomalies
CO2 Sources
Figure 6.26
GCM Model
2070-2100 Temperature ForecastVersus 1961-1990 Global Average
Figure 6.28
“You want proof?”
Figure 6.29
Then there’s the other side of the argument…
Stephen Schneider (1945-2010) Comments on the Climate Change Debate…
What thinkest thou?