8.2-kiloyear event wikipedia - EAS

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    SECUREen.wikipedia.org/wiki/8.2-kiloyear_event

    In climatology, the so-called "8.2-kiloyear event" was a sudden decrease in global temperatures that occurred approximately 8,200 years "BP", or c. 6,200 BC. It defines the start of the Northgrippian age in the Holocene epoch. Milder than the Younger Dryas cold period before it but more severe than

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    A rapid cooling around 6200 BC was first identified by Swiss botanist Heinrich Zoller in 1960, who named the event the Misox oscillation (for the Val Mesolcina). It is also known as the Finse event in Norway. Bond et al. argued that the

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    The event may have been caused by a large meltwater pulse from the final collapse of the Laurentide Ice Sheet of northeastern North America, most likely when the glacial lakes Ojibway and Agassiz suddenly drained into the North Atlantic Ocean. The same type of

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    Drier conditions were notable in North Africa, and East Africa was significantly affected by five centuries of general drought. In West Asia, especially Mesopotamia, the 8.2-kiloyear event was a 300-year aridification and cooling episode, which may have provided

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    • Acosta; et al. (2018). "Climate change and peopling of the Neotropics during the Pleistocene-Holocene transition". Boletín de la Sociedad Geológica Mexicana. 70 (1): 1‒19. doi:10.18268/BSGM2018v70n1a1.

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  2. 8.2 kiloyear event — Wikipedia Republished // WIKI 2

    SECUREwiki2.org/en/8.2_kiloyear_event

    In climatology, the 8.2-kiloyear event was a sudden decrease in global temperatures that occurred approximately 8,200 years before the present, or c. 6,200 BC, and which lasted for the next two to four centuries. It defines the start of the Northgrippian age in the Holocene epoch. Milder than the Younger Dryas cold spell before it but more severe than the Little Ice Age after …

  3. SECUREwww.wikiwand.com/en/8.2-kiloyear_event

    8.2-kiloyear event - Wikiwand In climatology, the 8.2-kiloyear event was a sudden decrease in global temperatures that occurred approximately 8,200 years before the present, or c. 6,200 BC, and which lasted for the next two to four centuries. It defines the start of the Northgrippian age in the Holocene epoch.

  4. SECUREen.wikipedia.org/wiki/Talk:8.2-kiloyear_event
    • In the Cooling Even section, there's a bit that uses the phrase "Before Present" ("In Greenland, the event started at 8175 Before Present"). Now, that's four significant figures. Over the lifetime of this article, present is going to shift quite a bit. Either someone's going to have to keep editing that figure, or someone needs to tie that to an ac...
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    • SECUREen.wikipedia.org/wiki/4.2-kiloyear_event

      • 8.2-kiloyear event
      • African humid period
      • Bond event
      • Climate variability and change
      • Great Flood (China) (c. 2300–2200 BC)

      • Estimated Reading Time: 9 mins
      • SECUREinfogalactic.com/info/8.2_kiloyear_event

        The 8.2 kiloyear event is the term that climatologists have adopted for a sudden decrease in global temperatures that occurred approximately 8,200 years before the present, or c. 6,200 BCE, and which lasted for the next two to four centuries.

      • SECUREchiefio.wordpress.com/2011/12/13/8-2-kiloyear-event-and-you

        Dec 13, 2011 · The 8.2 kiloyear event is the term that climatologists have adopted for a sudden decrease in global temperatures that occurred approximately 8,200 years before the present, or c. 6,200 BC, and which lasted for the next two to four centuries.

      • 8.2 Kiloyear Event | 82 Kiloyear Event - liquisearch.com

        SECUREwww.liquisearch.com/82_kiloyear_event

        The 8.2 kiloyear event is the term that climatologists have adopted for a sudden decrease in global temperatures that occurred approximately 8,200 years before the present, or c. 6,200 BCE, and which lasted for the next two to four centuries.

      • SECUREen.wikipedia.org/wiki/Bond_event

        Bond events are North Atlantic ice rafting events that are tentatively linked to climate fluctuations in the Holocene.Eight such events have been identified. Bond events were previously believed to exhibit a roughly c. 1,500-year cycle, but the primary period of variability is now put at c. 1,000 years.. Gerard C. Bond of the Lamont–Doherty Earth Observatory at Columbia University was …

      • Earth:4.2 kiloyear event - HandWiki

        SECUREhandwiki.org/wiki/Earth:4.2_kiloyear_event

        Aug 29, 2021 · The 4.2-kiloyear BP aridification event was one of the most severe climatic events of the Holocene epoch. It defines the beginning of the current Meghalayan age in the Holocene epoch.. Starting around 2200 BC, it probably lasted the entire 22nd century BC. It has been hypothesised to have caused the collapse of the Old Kingdom in Egypt as well as the Akkadian …

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