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The retreat of glaciers since 1850 is a well-documented effect of climate change. The retreat of mountain glaciers provide evidence for the rise in global temperatures since the late 19th century. Examples include mountain glaciers in western North America, Asia, the Alps in central Europe, and tropical and subtropical regions of South America ...
Knowledge of precise climatic events decreases as the record goes further back in time. The timeline of glaciation covers ice ages specifically, which tend to have their own names for phases, often with different names used for different parts of the world. The names for earlier periods and events come from geology and paleontology.
[6] [7] Since the end of the Last glacial period about 12,000 years ago, ice sheets have retreated on a global scale, and Earth has been experiencing a relatively warm interglacial period marked by only high-altitude alpine glaciers at most latitudes with larger ice sheet and sea ice at the poles. [8]
The retreat of glaciers since 1850 is well documented and has become an increasingly important climatic issue. Since the end of the Little Ice Age around the year 1850, glaciers worldwide have been retreating. This reduction in the mass of glaciers, referred to by glaciologists as glacier retreat, has been attributed primarily to global climate ...
The comparison found that the rate of glacial retreat in Greenland during the 21st century has been twice as fast as the retreat in the 20th century. Thousands of Greenland’s glaciers are ...
The Holocene glacial retreat is a geographical phenomenon that involved the global retreat of glaciers (deglaciation) that previously had advanced during the Last Glacial Maximum. Ice sheet retreat initiated ca. 19,000 years ago and accelerated after ca. 15,000 years ago.
Scientists explain the loss of the Humboldt Glacier in Venezuela's Sierra Nevada, which they believe makes the South American country the first in modern history to lose all its glaciers.
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