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Climate: Causes and Classification
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What is CLIMATE? Long-term weather patterns for an area (climatology) Variations in temperature, precipitation, and winds throughout the year
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What causes CLIMATE? An area’s climate is caused by a combination of 4 factors: Latitude Topographic Effects Air masses Side of Mountain Range
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1st Cause of Climate: Latitude
Most important cause! The latitude (how far North or South of the equator) determines how much solar radiation an area receives due to Earth’s tilt Equator = little tilt = high direct sunlight Poles = high tilt = little direct sunlight
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2nd Cause of Climate: Topographic Effects
Land vs. Water (distance to water) Coastal areas = wetter and moderate temperatures Inland areas = drier and more extreme temperatures Elevation Mountains = cooler Lower elevations = warmer
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3rd Cause of Climate: Air Masses
Same types of air masses move into the same area at the same time each year Air masses bring the characteristics of their source regions (cP, mT, etc) Air masses moving in interact with the air masses present to influence climate
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4th Cause of Climate: Side of Mountain Range
Windward Side Moist air rises over a mountain & cools at the top Wet climate forms Leeward Side Cold, dry air sinks down from the mountain & warms at the bottom Dry/Desert climate forms
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Koppen Classification System
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Koppen Classification System
Uses average monthly and annual values of temperature, precipitation, and vegetation to classify climates
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Koppen Classification System
Contains ~5 main divisions: Humid Tropical Dry Humid Mid-Latitude Continental Polar
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Koppen Classification System: Humid Tropical Climates
Constant high temperatures – no change in seasons Constant high humidity High amounts of precipitation Near the equator
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Koppen Classification System: Dry Climates
Little to no precipitation Hot summers & cool winters Subtypes: Arid (desert) Semi-arid
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Koppen Classification System: Humid Mid-Latitude Climates
Mild winters & warm, humid summers Abundant (lots of) rain Subtypes: Marine Humid subtropical Mediterranean
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Koppen Classification System: Continental
Severe winters & mild summers Primarily (mostly) located north of the equator Subtypes: Temperate Highlands
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Koppen Classification System: Polar Climates
Coldest regions on Earth (year-round) Little precipitation Winter days are (almost) all darkness; summer days (almost) all daylight Antarctica
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