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(4.4) Climates & Biomes: Cold
Jun 28, 2024
Climate Classification Lecture Notes
Introduction
Final lecture on Climate Classification
Upcoming topics:
Paleoclimate (historical climate change)
Modern day climate change
Severe Mid Latitude Climates (Capital D Classification)
Key Characteristics
Distinguished by a colder month with temperatures below freezing (< 32°F)
Must have at least one month warmer than 50°F
Term often used:
Severe Mid Latitudes
(also referred to as Microthermal)
Examples
Locations: Milwaukee, New York City, Great Lakes areas
Winter: Very cold
Summer: Warmer than some other colder regions
Biomes:
Deciduous and mixed conifer forests
Typical vegetation: Pine, Spruce, Deciduous trees
Outdoor recreational activities: Hunting, fishing
Agricultural Impact
Bread Basket of the United States
Crops: Corn, wheat, soybeans
Soils:
Mollisols
(rich, dark soil, good for grasslands)
Alfisols
(less organic material but mineral-rich, good for forests)
Moving North: Taiga Biome
Higher latitude: 50° to 70° north
Temperature: Extensive periods below freezing
Vegetation: Coniferous trees
Permafrost: Continuous or sporadic permafrost, affects soil stability
Polar Climates
Characteristics
Warmest month temperature < 50°F
Examples: Tundra and Ice Cap climates
Tundra Climate
Latitude: around 71° north
Temperature: Below 50°F on average, but some summer melt
Vegetation and Fauna: Lichens, arctic foxes, polar bears, reindeer, seals
Ice Cap Climate
Examples: Central Greenland, Antarctica
Year-round ice cover, no significant summer melt
Highland Climates
Characteristics
Associated with elevation differences (relief)
Climate affected by altitude and topography
Vary based on starting climate (desert, tropical, etc.) and elevation
Examples
Lower zones: Desert or tropical climates
Higher zones: May reach polar or ice cap climates
Diverse biomes: Depending on elevation range
Summary
Review different climate classifications and associated biomes
Understand temperature ranges and vegetation types for each classification
Upcoming focus on historical climate and modern climate change
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Full transcript