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Return to Physical Geography 5e Student Resources
Unit 18 Review Questions
Quiz Content
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When did humans first begin to have a major impact on climate change?
Around 200 A.D. at the height of the Roman Empire
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Around 1500 A.D. as colonial expansion began
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In the mid-1700s at the beginning of the Industrial Revolution
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In the mid-twentieth century with a major expansion of global population
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On a time scale of billions of years, which of the following best describes Earth's climate?
Ice-house climate
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Hot-house climate
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Snowball Earth
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Glacial/interglacial climate
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What drives glacial/interglacial cycles?
Volcanic outgassing of carbon dioxide
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Fluctuations in the Sun's output of solar radiation
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Milankovitch cycles
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Carbon dioxide-weathering feedback
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Water molecules containing O-18:
move faster at the same temperature than do water molecules containing O-16
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are found almost exclusively in the ocean
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evaporate at a slightly lower rate than water molecules containing O-16
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were present in the first billion years of Earth's history, but are now rare
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Carbon dioxide-weathering feedback leads to warmer temperatures when:
chemical weathering increases
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precipitation decreases
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continents shift toward the poles
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incoming solar radiation decreases
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Ice-albedo feedback:
amplifies warming only
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amplifies cooling only
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amplifies both warming and cooling
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suppresses warming and amplifies cooling
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Regarding climate change, negative feedback:
amplifies the initial change
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is quite rare compared to positive feedback
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leads to a progressively cooler climate
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has a stabilizing effect on climate
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The Little Ice Age:
brought temperatures that were lower than the previous glacial maximum
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led Vikings to move to Greenland
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began around 1100 A.D.
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was global in scope
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Snowball Earth:
has its effects reduced through ice-albedo feedback
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occurs about every 100 million years
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amplifies carbon dioxide-weathering feedback
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is evidenced by glacial deposits at tropical latitudes
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Why is the carbon dioxide-weathering feedback not a good solution for human-induced global warming?
It occurs on too slow a time scale.
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The continents are not well positioned for high rates of chemical weathering.
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Carbon dioxide-weathering feedback is only effective to stop cooling.
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The oceans now have a greatly reduced capacity to absorb carbon dioxide.
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