Predicted climate changes
Although the Earth's climate is naturally changeable, with fluctuations of up to 2°C per century (IPCC, 1990), human emissions of a number of gases (the ‘greenhouse gases’), including carbon dioxide (CO 2), methane (CH4), halocarbons (CFCs and HCFCs) and nitrous oxide (N2O), are likely to create changes in climate that are much more rapid than those experienced in human history. With the exception of halocarbons, greenhouse gases occur naturally; in fact, without them the mean surface temperature of the Earth would be –15°C (IPCC, 1990). However, human activities have increased the atmospheric concentrations of these gases. creating the ‘enhanced greenhouse effect.’ This is expected to increase mean surface temperature between 1.5°C and 4.5°C by the middle of the 21st century, with a best estimate of a global mean warming of 2.5°C (Houghton et al., 1992). In the absence of controls on greenhouse gas emissions, the rate of warming will be about 0.3°C per...
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Cross-references
Carbon-14 Dating; Climatic Modeling; Cycles, Climatic; Dendrochronology; El Niño–Southern Oscillation (ENSO); Glaciers, Glaciology; Global Change; Global Climatic Change Modeling and Monitoring; Greenhouse Effect; Ice Ages; Lichens, Lichenometry; Ozone; Sunspots, Environmental Influence; Paleoecology; Radioisotopes, Radionuclides; Sea-Level Change; Solar Cycle; Zones, Climatic
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Herbert, D., Burton, I. (1999). Climate change. In: Environmental Geology. Encyclopedia of Earth Science. Springer, Dordrecht. https://doi.org/10.1007/1-4020-4494-1_56
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DOI: https://doi.org/10.1007/1-4020-4494-1_56
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