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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 ...
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.
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 ...
Retrieved from "https://en.wikipedia.org/w/index.php?title=Glacial_retreat&oldid=1024723398"This page was last edited on 23 May 2021, at 19:43
The Extreme Ice Survey (EIS), based in Boulder, Colorado, uses time-lapse photography, conventional photography and video to document the effects of global warming on glacial ice. It is the most wide-ranging glacier study ever conducted using ground-based, real-time photography.
Retreat of glaciers since 1850 – Recent shrinking of glaciers due to global warming; Timeline of glaciation – Chronology of the major ice ages of the Earth; Younger Dryas – Time period c. 12,900–11,700 years ago with Northern Hemisphere glacial cooling and SH warming
Glacier retreat primarily refers to the retreat of glaciers since 1850. It may also refer to: Glacial retreat, a type of glacial motion; Deglaciation, the widespread retreat of glaciers at the end of an ice age; Holocene glacial retreat, a period of deglaciation occurring between 20,000 and 10,000 years ago
During that time period, glaciers moved down to as low as 9,200 feet (2,800 m), but subsequent warming during the Holocene Epoch (starting 10,000 years ago) caused widespread melting of both continental glaciers and other alpine glaciers. Specifically, there has been a global retreat of glaciers since 1850. Given current warming trends, the ...