Matches in SemOpenAlex for { <https://semopenalex.org/work/W323362739> ?p ?o ?g. }
- W323362739 endingPage "134" @default.
- W323362739 startingPage "126" @default.
- W323362739 abstract "The Younger Dryas is the last major abrupt climate change event of the last deglaciation occurring ~12 900–11 700 years ago. Large portions of the Northern Hemisphere cooled and much of the Southern Hemisphere warmed during the event in a bipolar seesaw pattern. While changes in net precipitation were more variable at higher latitudes, Northern Hemisphere subtropics and tropics were generally drier and the Southern Hemisphere subtropics wetter from southward migration of the Intertropical Convergence Zone. Many of the climate changes related to the Younger Dryas were likely a response to increased freshwater discharge to the North Atlantic and the attendant reduction in Atlantic meridional overturning strength. Although multiple freshwater forcing hypotheses have been proposed, the existing terrestrial and marine records indicate that the northward retreat of the southern margin of the Laurentide Ice Sheet from the Great Lakes caused a routing of freshwater from the western Canadian Plains from the Mississippi River to the St. Lawrence River, with the increased freshwater discharge to the North Atlantic slowing ocean circulation and ultimately causing the Younger Dryas." @default.
- W323362739 created "2016-06-24" @default.
- W323362739 creator A5026025165 @default.
- W323362739 date "2013-01-01" @default.
- W323362739 modified "2023-10-10" @default.
- W323362739 title "PALEOCLIMATE | The Younger Dryas Climate Event" @default.
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