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Understanding Our Environment
Understanding Our Environment

... Ice cores - collected from glaciers reveal light and dark bands caused by annual snow accumulation on glacier  Gas bubbles can be analyzed for atmospheric composition.  Ash and sulfur deposits correlate with volcanic eruptions.  Vostok ice core gives us a record back 420,000 years. ...
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Ch.19 APES Study Guide: Global Warming and Ozone Loss
Ch.19 APES Study Guide: Global Warming and Ozone Loss

... 7. Describe the period the earth has been experiencing for the last 10,000 years. 8. Describe the general trend of mean global temperature since 1860. List two factors other than the greenhouse effect that may have contributed to the general temperature change. 9. State the consensus science view ab ...
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Climate change feedback



Climate change feedback is important in the understanding of global warming because feedback processes may amplify or diminish the effect of each climate forcing, and so play an important part in determining the climate sensitivity and future climate state. Feedback in general is the process in which changing one quantity changes a second quantity, and the change in the second quantity in turn changes the first. Positive feedback amplifies the change in the first quantity while negative feedback reduces it.The term ""forcing"" means a change which may ""push"" the climate system in the direction of warming or cooling. An example of a climate forcing is increased atmospheric concentrations of greenhouse gases. By definition, forcings are external to the climate system while feedbacks are internal; in essence, feedbacks represent the internal processes of the system. Some feedbacks may act in relative isolation to the rest of the climate system; others may be tightly coupled; hence it may be difficult to tell just how much a particular process contributes. Forcings, feedbacks and the dynamics of the climate system determine how much and how fast the climate changes. The main positive feedback in global warming is the tendency of warming to increase the amount of water vapor in the atmosphere, which in turn leads to further warming. The main negative feedback comes from the Stefan–Boltzmann law, the amount of heat radiated from the Earth into space changes with the fourth power of the temperature of Earth's surface and atmosphere.Some observed and potential effects of global warming are positive feedbacks, which contribute directly to further global warming. The Intergovernmental Panel on Climate Change's (IPCC) Fourth Assessment Report states that ""Anthropogenic warming could lead to some effects that are abrupt or irreversible, depending upon the rate and magnitude of the climate change.""
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