Holocene Temperature Variations

The Piora Oscillations are two cold periods in the Alpine climate history of the Holocene Epoch. Its dating differs between authors and no consistent modern approach currently exists. The spatial extent of the change is unclear; moreover, it does not show up as a major, or even identifiable, event in hemispheric temperature reconstructions.[citation needed]

The phenomenon is named after the Val Piora (Piora Valley) in Switzerland, where it was first detected.

See also

Notes

  • Baronia, Carlo; Orombelli, Giuseppe (1996). "The Alpine "Iceman" and Holocene Climatic Change". Quaternary Research. 46 (1): 78–83. Bibcode:. doi:. S2CID .
  • Burroughs, William J. (2003). . Cambridge: Cambridge University Press. ISBN 0-521-79202-9.
  • Caseldine, C.; Thompson, G.; Langdon, C.; Hendon, D. (2005). "Evidence for an extreme climatic event on Achill Island, Co. Mayo, Ireland around 5200–5100 cal. yr BP". Journal of Quaternary Science. 20 (2): 169–178. Bibcode:. doi:. S2CID .
  • Hou, Mei; Wu, Wen Xiang (5 December 2020). . Quaternary International. 571: 58–72. doi:. ISSN .
  • Lamb, Hubert H. (1995). . London: Routledge. ISBN 0-415-12735-1.
  • Magny, Michel; Haas, Jean Nicolas (2004). . Journal of Quaternary Science. 19 (5): 423–430. Bibcode:. doi:. S2CID .
  • Matossian, Mary A. K. (1997). . New York: M. E. Sharpe. ISBN 0-7656-0061-7.
  • Wick, Lucia; Tinner, Willy (1997). "Vegetation Changes and Timberline Fluctuations in the Central Alps as Indicators of Holocene Climatic Oscillations". Arctic and Alpine Research. 29 (4): 445–458. doi:. JSTOR .