Coconote
AI notes
AI voice & video notes
Export note
Try for free
(4.1) Climate Classification and Biomes
Jun 28, 2024
Climate Classification and Biomes
Introduction
Regional issues, long-term changes, distribution of climates in the US and globally
Goal: Interpret and explain a climate classification chart
Climate Classification
Data Used: Temperature and Precipitation Patterns
Earth-Sun Relationships: Latitude Impact
Average temperature decreases moving towards poles
Greater temperature spread away from the equator
Other Influences on Climate
Solar angle, incoming solar radiation
Specific heat, heat capacity (e.g., proximity to oceans vs. continental interiors)
Temperature Classifications
Moving away from equator: Increased seasonality, higher temperature ranges
Interior continents: Can get very warm or very cold due to lack of moderating ocean influence
Precipitation Classifications
Annual Rainfall and Seasonal Patterns
Some regions have distinct wet/dry seasons
Precipitation Lifting Mechanisms
ITCZ (Inter-Tropical Convergence Zone): High precipitation
Orographic Uplift: Windward side wet, leeward side dry
Continental Interiors: Generally drier due to lack of moisture source
High Precipitation Regions
Amazon rainforest, Southeastern Asia monsoons
Low Precipitation Regions
Deserts (Namib, Sahara, Atacama, Outback, Desert Southwest in the US)
Subtropical and Polar Regions
: Dominated by high pressure, generally drier
Air Masses and Climates
Air masses dominate regional climates
Examples:
Gulf Coast (MT air masses)
Desert Southwest (CT air masses)
Northern regions (CP air masses)
Seasonality Impact
Important to differentiate consistent precipitation vs. seasonal variations (e.g., monsoon climates)
Koppen Climate Classification System
Focus on names of climates, not letter designations
Letters help map climates but real-world understanding is based on climate names (Rainforest, Desert, Mediterranean, etc.)
Climate names relate to biomes and dominant plant life
Biomes
Named for prevailing climate and dominant vegetation
High correlation between climate and natural vegetation
Examples:
Tropical Rainforest
: Central America, South America, parts of Africa, Southeastern Asia
Deserts
: Atacama, Southwest US, Sahara
Tundra
: Extremely cold, minimal vegetation
Taiga
: Coniferous forest belt
North America Examples
Southeastern US: MT air mass, similar vegetation (East Texas to Georgia)
Marine rainforest in Pacific Northwest
Warm and cool deserts in the Southwest
Deciduous and coniferous mixed forests in the northern regions
Climate, Soil Development, and Vegetation
Temperature and Aridity
: Key factors in climate classification
Soil Types Related to Climate
Example: Grassland soils: Rich in organic matter, good for crops
Arid soils: Low organic matter, high in calcium carbonate
Climate Graphs (Climographs)
Components
Line graph: Temperature
Bar graph: Precipitation
Example: Houston, Texas
Temperature never drops below freezing
50 inches of annual rain
Understanding Houston's climate helps in comparing other climates
Key Takeaways
Importance of understanding climate graphs
Use of temperature and precipitation to classify climates
Relate climate data to real-world examples and biomes
Next lectures: Detailed climate classifications and associated biomes
📄
Full transcript