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- Neoglaciation abstract "The neoglaciation ("renewed glaciation") describes the documented cooling trend in the Earth's climate during the Holocene, following the retreat of the Wisconsin glaciation, the most recent glacial period. Neoglaciation has followed the hypsithermal or Holocene Climatic Optimum, the warmest point in the Earth's climate during the current interglacial stage. The neoglaciation has no well-marked universal beginning: local conditions and ecological inertia affected the onset of detectably cooler (and wetter) conditions. Driven inexorably by the Milankovitch cycle, cooler summers in higher latitudes of North America, which would cease to completely melt the annual snowfall, were masked at first by the presence of the slowly disappearing continental ice sheets, which persisted long after the astronomically calculated moment of maximum summer warmth: "the neoglaciation can be said to have begun when the cooling caught up with the warming", remarked E. C. Pielou. With the close of the "Little Ice Age" (mid-14th to late 19th centuries), neoglaciation appears to have been stalled in the late 20th century, assumed to be caused by anthropogenic global warming. Whether it has been temporarily or semi-permanently stalled, neoglaciation has been marked by a retreat from the warm conditions of the Climatic Optimum and the advance or reformation of glaciers that had not existed since the last ice age. In the mountains of western North America, montane glaciers that had completely melted reformed shortly before 5000 BP. The most severe part of the best documented neoglacial period, especially in Europe and the North Atlantic, is termed the "Little Ice Age".In North America, neoglaciation had ecological effects in the spread of muskeg on flat, poorly drained land, such as the bed of recently drained Lake Agassiz and in the Hudson Bay lowlands, in the retreat of grassland before an advancing forest border in the Great Plains, and in shifting ranges of forest trees and diagnostic plant species (identified through palynology). The view that neoglaciation is ending in present times, is assumed by those who identify the most recent climate changes and global warming as the onset of a new period in Earth history, speculatively calling it the "Early anthropocene", as a coming geological age dominated by the effects of Homo sapiens.".
- Neoglaciation wikiPageID "11089071".
- Neoglaciation wikiPageLength "3786".
- Neoglaciation wikiPageOutDegree "33".
- Neoglaciation wikiPageRevisionID "633550237".
- Neoglaciation wikiPageWikiLink Before_Present.
- Neoglaciation wikiPageWikiLink Category:Climate.
- Neoglaciation wikiPageWikiLink Category:Climate_history.
- Neoglaciation wikiPageWikiLink Category:Holocene.
- Neoglaciation wikiPageWikiLink Climatology.
- Neoglaciation wikiPageWikiLink E._C._Pielou.
- Neoglaciation wikiPageWikiLink Early_anthropocene.
- Neoglaciation wikiPageWikiLink Earth_history.
- Neoglaciation wikiPageWikiLink Ecological_stability.
- Neoglaciation wikiPageWikiLink Glacial_period.
- Neoglaciation wikiPageWikiLink Glaciation.
- Neoglaciation wikiPageWikiLink Glacier.
- Neoglaciation wikiPageWikiLink Global_warming.
- Neoglaciation wikiPageWikiLink Great_Plains.
- Neoglaciation wikiPageWikiLink History_of_Earth.
- Neoglaciation wikiPageWikiLink Holocene.
- Neoglaciation wikiPageWikiLink Holocene_Climatic_Optimum.
- Neoglaciation wikiPageWikiLink Holocene_climatic_optimum.
- Neoglaciation wikiPageWikiLink Homo_sapiens.
- Neoglaciation wikiPageWikiLink Hudson_Bay.
- Neoglaciation wikiPageWikiLink Human_impact_on_the_environment.
- Neoglaciation wikiPageWikiLink Hypsithermal.
- Neoglaciation wikiPageWikiLink Ice_age.
- Neoglaciation wikiPageWikiLink Interglacial.
- Neoglaciation wikiPageWikiLink Lake_Agassiz.
- Neoglaciation wikiPageWikiLink Last_glacial_period.
- Neoglaciation wikiPageWikiLink Little_Ice_Age.
- Neoglaciation wikiPageWikiLink Milankovitch_cycle.
- Neoglaciation wikiPageWikiLink Milankovitch_cycles.
- Neoglaciation wikiPageWikiLink Muskeg.
- Neoglaciation wikiPageWikiLink Palynology.
- Neoglaciation wikiPageWikiLink Principle_of_faunal_succession.
- Neoglaciation wikiPageWikiLink Wisconsin_glaciation.
- Neoglaciation wikiPageWikiLinkText "Neoglacial".
- Neoglaciation wikiPageWikiLinkText "Neoglaciation".
- Neoglaciation wikiPageWikiLinkText "changing climatic conditions".
- Neoglaciation wikiPageWikiLinkText "neoglaciation".
- Neoglaciation hasPhotoCollection Neoglaciation.
- Neoglaciation wikiPageUsesTemplate Template:Reflist.
- Neoglaciation subject Category:Climate.
- Neoglaciation subject Category:Climate_history.
- Neoglaciation subject Category:Holocene.
- Neoglaciation comment "The neoglaciation ("renewed glaciation") describes the documented cooling trend in the Earth's climate during the Holocene, following the retreat of the Wisconsin glaciation, the most recent glacial period. Neoglaciation has followed the hypsithermal or Holocene Climatic Optimum, the warmest point in the Earth's climate during the current interglacial stage.".
- Neoglaciation label "Neoglaciation".
- Neoglaciation sameAs Uusjäätumine.
- Neoglaciation sameAs ネオグラシエーション.
- Neoglaciation sameAs Neoglasiasjon.
- Neoglaciation sameAs m.02q_ny0.
- Neoglaciation sameAs Q3739003.
- Neoglaciation sameAs Q3739003.
- Neoglaciation wasDerivedFrom Neoglaciation?oldid=633550237.
- Neoglaciation isPrimaryTopicOf Neoglaciation.