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Geology 1001/1101
Sec 003 Chris PaolaClass 12: climate and glaciation
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Chapter 10
THE CLIMATE SYSTEM
AND GLACIATION
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Key ideas about climate & glaciation
• Much of Minnesota’s landscape has been sculpted by glaciers
• Glacial cycles are controlled by variation in Earth’s orbit on time scales of 10,000 – 100,000 yr
• Climate weather; climate is long-term average of weather
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Climate: planetary controls
• Distance from Sun
• Albedo (reflectivity or “whiteness”)
• Atmosphere (greenhouse effect)
• Orbital properties
• Plate configuration (mainly due to effect on ocean circulation)
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Climate: geographic controls
• Distance from equator
• Average air flow & pressure
• Distance to the ocean
• Prevailing wind relative to mountains & ocean
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Hot
Cold
NOT distance to Sun!
3,900 miles
92,900,000 miles
7all sunlight that hits Earth’s surface
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10% of sunlight spread across 6.5% of sunlit surface
at equator, Earth’s surface is almost perpendicular to sunlight, so energy is concentrated in small area
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10% of sunlight spread across 6.5% of sunlit surface
~ 150% of average intensity
at equator, Earth’s surface is almost perpendicular to sunlight, so energy is concentrated in small area
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10% of sunlight spread across 6.5% of sunlit surface
10% of sunlight spread across 20.5% of sunlit surface
~ 150% of average intensity
at poles, Earth’s surface slopes away from sunlight, so energy is spread across a greater area
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10% of sunlight spread across 6.5% of sunlit surface
10% of sunlight spread across 20.5% of sunlit surface
~ 150% of average intensity
< 50% of average intensity
at poles, Earth’s surface slopes away from sunlight, so energy is spread across a greater area
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Hot
Cold
due to the angle of the Earth’s surface
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Global air flow determines large-scale rainfall patterns