Chapter 19 Review

chapter 19Review

In this chapter, we learned the distinctions among global change, global climate change, and global warming. Global warming is an inherently natural process whereby a tiny percentage of gases in the atmosphere, known as greenhouse gases, absorb infrared radition from Earth and emit some of this energy back to Earth. This warms the planet. Environmental scientists are concerned that human activities have caused a higher concentration of greenhouse gases in the atmosphere that is responsible for a gradual warming of the planet above that observed a century ago. The average amount of warming around the world has been relatively small at 0.8°C but some regions such as high northern latitudes have experienced increases of up to 4°C. This warming has caused a decline in polar ice, a decline in glaciers, an increased thawing of permafrost, and an increase in sea level. It has also affected the timing of plant flowering, bird migration, insect emergence, and the length of growing seasons. While these effects have already been observed, other climate changes are also predicted to occur including more extreme temperatures, more instense storms, changing patterns of precipitation, and altered ocean current. The Kyoto Protocol was designed to reduce the global emissions of greenhosue gases, but the goal set by nations around the world has not yet been achieved.

Key Terms

Question

Global change
Global climate change
Global warming
Greenhouse effect
Greenhouse warming potential
Ocean acidification
Kyoto Protocol
Carbon sequestration
An international agreement that sets a goal for global emissions of greenhouse gases from all industrialized countries to be reduced by 5.2 percent below their 1990 levels by 2012.
The warming of the oceans, land masses, and atmosphere of Earth.
Change that occurs in the chemical, biological, and physical properties of the planet.
An estimate of how much a molecule of any compound can contribute to global warming over a period of 100 years relative to a molecule of CO2.
The process by which an increase in ocean CO2 causes more CO2 to be converted to carbonic acid, which lowers the pH of the water.
Absorption of infrared radiation by atmospheric gases and reradiation of the energy back toward Earth.
An approach to stabilizing greenhouse gases by removing CO2 from the atmosphere.
Changes in the average weather that occurs in an area over a period of years or decades.

Learning Objectives Revisited

Page 697

Module 62 Global Climate Change and the Greenhouse Effect

Module 63 The Evidence for Global Warming

Module 64 The Consequences of Global Climate Change

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