Climate+change

 Encyclopædia Britannica ||
 * =climate change =


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//1938-T.J. Hileman/Glacier National Park Archives, 1981 - Carl Key/USGS, 1998 - Dan Fagre/USGS, 2006 - Karen Holzer/USGS// || periodic modification of Earth's climate brought about as a result of changes in the atmosphere as well as interactions between the atmosphere and various other geologic, chemical, biological, and geographic factors within the Earth system. The atmosphere is a dynamic fluid that is continually in motion. Both its physical properties and its rate and direction of motion are influenced by a variety of factors, including solar radiation, the geographic position of continents, ocean currents, the location and orientation of mountain ranges, atmospheric chemistry, and vegetation growing on the land surface. All these factors change through time. Some factors, such as the distribution of heat within the oceans, atmospheric chemistry, and surface vegetation, change at very short timescales. Others, such as the position of continents and the location and height of mountain ranges, change over very long timescales. Therefore, climate, which results from the physical properties and motion of the atmosphere, varies at every conceivable timescale. Climate is often defined loosely as the average weather at a particular place, incorporating such features as temperature, precipitation, humidity, and windiness. A more specific definition would state that climate is the mean state and variability of these features over some extended time period. Both definitions acknowledge that the weather is always changing, owing to instabilities in the atmosphere. And as weather varies from day to day, so too does climate vary, from daily day-and-night cycles up to periods of geologic time hundreds of millions of years long. In a very real sense, //climate variation// is a redundant expression—climate is always varying. No two years are exactly alike, nor are any two decades, any two centuries, or any two millennia. This article addresses the concept of climatic variation and change within the set of integrated natural features and processes known as the Earth system. The nature of the evidence for climate change is explained, as are the principal mechanisms that have caused climate change throughout the history of Earth. Finally, a detailed description is given of climate change over many different timescales, ranging from a typical human life span to all of geologic time. For a detailed description of the development of Earth's atmosphere, //see// the article atmosphere, evolution of. For full treatment of the most critical issue of climate change in the contemporary world, //see// global warming. == == > Encyclopædia Britannica, Inc., 2011. Web. 13 Sept. 2011.
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 * [[image:http://cache.eb.com/eb/thumb?id=112550 width="100" height="35" caption="Photograph:A series of photographs of the Grinnell Glacier taken from the summit of Mount Gould in Glacier …"]]|| A series of photographs of the Grinnell Glacier taken from the summit of Mount Gould in Glacier …
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 * " **climate change .**" //Encyclopædia Britannica//. //Encyclopædia Britannica Online Library Edition//.