Describe the greenhouse effect and why increasing greenhouse gases leads to warming.

Prepare for the Earth and Environment (ESC 102) Test with tailored flashcards and multiple-choice questions. Each question includes hints and explanations to ensure your success. Get exam-ready now!

Multiple Choice

Describe the greenhouse effect and why increasing greenhouse gases leads to warming.

Explanation:
The essential idea is that greenhouse gases trap heat. Solar radiation from the sun arrives mainly as visible light and heats the Earth's surface. That surface then emits infrared radiation as heat. Greenhouse gases—like carbon dioxide, methane, and nitrous oxide—are efficient at absorbing this infrared radiation. When they absorb it, the molecules vibrate and re-emit infrared energy in all directions, including back toward the surface. This trapping of heat slows the loss of energy to space, warming the air near the surface and the lower atmosphere. When human activities raise the concentrations of these gases, more infrared energy is absorbed and re-emitted downward, boosting the surface temperature. These gases don’t block sunlight or reflect visible light, so they don’t cool the surface in the way some people imagine. Their warming effect comes from absorbing infrared radiation, not from blocking visible light, and their impact is strongest in the lower atmosphere and at the surface rather than being confined to the stratosphere.

The essential idea is that greenhouse gases trap heat. Solar radiation from the sun arrives mainly as visible light and heats the Earth's surface. That surface then emits infrared radiation as heat. Greenhouse gases—like carbon dioxide, methane, and nitrous oxide—are efficient at absorbing this infrared radiation. When they absorb it, the molecules vibrate and re-emit infrared energy in all directions, including back toward the surface. This trapping of heat slows the loss of energy to space, warming the air near the surface and the lower atmosphere. When human activities raise the concentrations of these gases, more infrared energy is absorbed and re-emitted downward, boosting the surface temperature.

These gases don’t block sunlight or reflect visible light, so they don’t cool the surface in the way some people imagine. Their warming effect comes from absorbing infrared radiation, not from blocking visible light, and their impact is strongest in the lower atmosphere and at the surface rather than being confined to the stratosphere.

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