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Younger Dryas information


Evolution of temperatures in the postglacial period, after the Last Glacial Maximum, showing very low temperatures for the most part of the Younger Dryas, rapidly rising afterwards to reach the level of the warm Holocene, based on Greenland ice cores.[1]

The Younger Dryas, which occurred circa 12,900 to 11,700 years Before Present (BP),[2] was a stadial (cooling) event which marked a return to glacial conditions, temporarily reversing the climatic warming of the preceding Late Glacial Interstadial (also known as the Bølling–Allerød interstadial, which spanned from 14,670 to 12,900 BP.).[3] The Younger Dryas was the most severe and longest lasting of several interruptions to the warming of the Earth's climate. The end of the Younger Dryas marks the beginning of the current Holocene epoch.

The change was relatively sudden, took place over decades, and resulted in a decline of temperatures in Greenland by 4–10 °C (7.2–18 °F),[4] and advances of glaciers and drier conditions over much of the temperate Northern Hemisphere. A number of hypotheses have been put forward about the cause, and the hypothesis historically most supported by scientists is that the Atlantic meridional overturning circulation, which transports warm water from the Equator towards the North Pole, was interrupted by an influx of fresh, cold water from North America into the Atlantic.[5] However, several issues do exist with this hypothesis, one of which is the lack of a clear geomorphological route for the meltwater. In fact, the originator of the meltwater hypothesis, Wallace Broecker, stated in 2010 that "The long-held scenario that the Younger Dryas was a one-time outlier triggered by a flood of water stored in proglacial Lake Agassiz has fallen from favor due to lack of a clear geomorphic signature at the correct time and place on the landscape".[6] A volcanic trigger has been proposed more recently,[7] and the presence of anomalously high levels of volcanism immediately preceding the onset of the Younger Dryas has been confirmed in both ice cores[8] and cave deposits.[9]

The Younger Dryas did not affect the climate equally worldwide, but the average worldwide temperature changed drastically. For example, in the Southern Hemisphere and some areas of the Northern Hemisphere, such as southeastern North America, a slight warming occurred.[10]

The Younger Dryas is named after an indicator genus, the alpine-tundra wildflower Dryas octopetala, as its leaves are occasionally abundant in late glacial, often minerogenic-rich sediments, such as the lake sediments of Scandinavia.

  1. ^ Zalloua & Matisoo-Smith 2017.
  2. ^ Rasmussen et al. 2006.
  3. ^ Clement & Peterson 2008.
  4. ^ Buizert, C.; Gkinis, V.; Severinghaus, J.P.; He, F.; Lecavalier, B.S.; Kindler, P.; et al. (5 September 2014). "Greenland temperature response to climate forcing during the last deglaciation". Science. 345 (6201): 1177–1180. Bibcode:2014Sci...345.1177B. doi:10.1126/science.1254961. ISSN 0036-8075. PMID 25190795. S2CID 206558186. Retrieved 18 September 2023.
  5. ^ Meissner, K.J. (2007). "Younger Dryas: A data to model comparison to constrain the strength of the overturning circulation". Geophysical Research Letters. 34 (21): L21705. Bibcode:2007GeoRL..3421705M. doi:10.1029/2007GL031304.
  6. ^ Broecker, Wallace S.; Denton, George H.; Edwards, R. Lawrence; Cheng, Hai; Alley, Richard B.; Putnam, Aaron E. (1 May 2010). "Putting the Younger Dryas cold event into context". Quaternary Science Reviews. 29 (9): 1078–1081. Bibcode:2010QSRv...29.1078B. doi:10.1016/j.quascirev.2010.02.019. ISSN 0277-3791.
  7. ^ Baldini, James U. L.; Brown, Richard J.; Mawdsley, Natasha (4 July 2018). "Evaluating the link between the sulfur-rich Laacher See volcanic eruption and the Younger Dryas climate anomaly". Climate of the Past. 14 (7): 969–990. Bibcode:2018CliPa..14..969B. doi:10.5194/cp-14-969-2018. ISSN 1814-9324.
  8. ^ Abbott, P.M.; Niemeier, U.; Timmreck, C.; Riede, F.; McConnell, J.R.; Severi, M.; Fischer, H.; Svensson, A.; Toohey, M.; Reinig, F.; Sigl, M. (December 2021). "Volcanic climate forcing preceding the inception of the Younger Dryas: Implications for tracing the Laacher See eruption". Quaternary Science Reviews. 274: 107260. Bibcode:2021QSRv..27407260A. doi:10.1016/j.quascirev.2021.107260.
  9. ^ Sun, N.; Brandon, A. D.; Forman, S. L.; Waters, M. R.; Befus, K. S. (31 July 2020). "Volcanic origin for Younger Dryas geochemical anomalies ca. 12,900 cal B.P." Science Advances. 6 (31): eaax8587. Bibcode:2020SciA....6.8587S. doi:10.1126/sciadv.aax8587. ISSN 2375-2548. PMC 7399481. PMID 32789166.
  10. ^ Carlson, A.E. (2013). "The Younger Dryas Climate Event" (PDF). Encyclopedia of Quaternary Science. Vol. 3. Elsevier. pp. 126–134. Archived from the original (PDF) on 11 March 2020.

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