In the distant geologic past, the temperature of Earth's atmosphere was the same worldwide.
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Q23: If Earth were to stop receiving energy
Q24: The most abundant component of Earth's atmosphere
Q25: Without greenhouse gasses, Earth's average air temperature
Q26: Worldwide seasonal effects in carbon dioxide in
Q27: Warm air is less dense than cold
Q29: Biologically important marine upwellings form when shallow
Q30: Carbon dioxide dissolves more readily in cold
Q31: Scandinavia has much less ice cover than
Q32: Earth's northern hemisphere has always had winter
Q33: Methane is a more potent greenhouse gas
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