Climate Stability on Earth and Earthlike Planets
Learning Objectives
After reading this chapter, students should be able to:
• Realize how the Sun and the Earth’s atmospheric composition have evolved over
timescales of billions of years.
• Know what the habitable zone of a star system is.
• Explain why Venus and Mars do not have liquid water at their surface.
• Know what the significance of the CO2 compensation point is.
• Describe how Venus developed a runaway greenhouse.
• Describe how Mars lost most of its atmosphere and surface water.
• Realize that astronomers have discovered over 100 extrasolar planets.
• Know how the continuously habitable zone is defined.
• Know what the Drake equation is, and be able to discuss the variables in the Drake
equation.
• Recognize how dependent the Drake equation is on the lifetime of advanced
civilizations.
• Understand the long-term threats to life and advanced civilization on Earth.
Review Questions
1.) How should future solar evolution affect climate and life here on Earth?
As the sun ages, it becomes brighter. This results in a higher incoming solar flux
at Earth orbit. The carbonate-silicate cycle dictates that this higher solar flux will
2.) What is the evidence that Venus once possessed more water than it does today?
How did it lose its water, and how did its atmosphere evolve afterward?
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