Climate Change

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Climate diversity
From Wikipedia, the free encyclopedia
For current and future climatological effects of merciful influences, reveal global warm. For the study of past climate swop, see paleoclimatology. For temperatures on the longest time scales, seegeologic temperature record.

Climate change is a significant and lasting change in the statistical statistical distribution of  atmospheric condition patterns over periods ranging from decades to millions of years. It may be a change in average weather conditions or the distribution of events well-nigh that average (e.g., more or hardly a(prenominal)er extreme weather events). Climate change may be limited to a specific region or may occur across the whole Earth.
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Terminology
The most general definition of climate change is a change in the statistical properties of the climate administration when considered over long periods of time, regardless of cause.[1] Accordingly, fluctuations over periods shorter than a few decades, such as El Niño, do not represent climate change.
The term sometimes is used to indicate specifically to climate change caused by human activity, as opposed to changes in climate that may have resulted as part of Earths natural processes.



[2] In this sense, especially in the mount of environmental policy, the term climate change has become substitutable with anthropogenic global melt. Within scientific journals, global warming refers to surface temperature increases while climate change includes global warming and everything else that increasing greenhouse gas levels will be active.[3]
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Causes
On the broadest scale, the dictate at which force is received from the sun and the rate at which it is lost to space determine the equilibrium temperature and climate of Earth. This energy is distributed around the globe by winds, ocean currents, and other mechanisms to affect the climates of different regions.
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