Younger Dryas - Global Effects

Global Effects

In western Europe and Greenland, the Younger Dryas is a well-defined synchronous cool period. But cooling in the tropical North Atlantic may have preceded this by a few hundred years; South America shows a less well defined initiation but a sharp termination. The Antarctic Cold Reversal appears to have started a thousand years before the Younger Dryas, and has no clearly defined start or end; Huybers has argued that there is fair confidence in the absence of the Younger Dryas in Antarctica, New Zealand and parts of Oceania. Timing of the tropical counterpart to the Younger Dryas – the Deglaciation Climate Reversal (DCR) – is difficult to establish as low latitude ice core records generally lack independent dating over this interval. An example of this is the Sajama ice core (Bolivia), for which the timing of the DCR has been pinned to that of the GISP2 ice core record (central Greenland). Climatic change in the central Andes during the DCR, however, was significant and characterized by a shift to much wetter, and likely colder, conditions. The magnitude and abruptness of these changes would suggest that low latitude climate did not respond passively during the YD/DCR.

In western North America it is likely that the effects of the Younger Dryas were less intense than in Europe; however, evidence of glacial re-advance indicates Younger Dryas cooling occurred in the Pacific Northwest.

Other features seen include:

  • Replacement of forest in Scandinavia with glacial tundra (which is the habitat of the plant Dryas octopetala).
  • Glaciation or increased snow in mountain ranges around the world.
  • Formation of solifluction layers and loess deposits in Northern Europe.
  • More dust in the atmosphere, originating from deserts in Asia.
  • Drought in the Levant, perhaps motivating the Natufian culture to develop agriculture.
  • The Huelmo/Mascardi Cold Reversal in the Southern Hemisphere ended at the same time.
  • Decline of the Clovis Culture and extinction of animal species in North America.

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