Potential for Southern Hemisphere climate surprises

P. A. Mayewski, T. Bracegirdle, I. Goodwin, D. Schneider, N. A.N. Bertler, S. Birkel, A. Carleton, M. H. England, J. H. Kang, A. Khan, J. Russell, J. Turner, I. Velicogna

Research output: Contribution to journalArticlepeer-review

19 Scopus citations

Abstract

Climate model results suggest that future climate change in Antarctica will be accompanied by continued strengthening and poleward contraction of the Southern Ocean westerly wind belt. Paleoclimate records suggest past changes in the westerly winds can be abrupt and that healing of the Antarctic ozone hole could lead to poleward contraction of the westerlies and increased meridional atmospheric transport of warm air regionally into Antarctica. An abrupt shift to more meridional circulation could lead to notable changes in moisture availability for extra-Antarctic regions, increased Antarctic ice sheet disintegration and more rapid sea-level rise.

Original languageEnglish (US)
Pages (from-to)391-395
Number of pages5
JournalJournal of Quaternary Science
Volume30
Issue number5
DOIs
StatePublished - Jul 1 2015

Keywords

  • Antarctica
  • Climate modeling
  • Paleoclimate
  • Southern Hemisphere climate
  • Westerlies

ASJC Scopus subject areas

  • Arts and Humanities (miscellaneous)
  • Earth and Planetary Sciences (miscellaneous)
  • Palaeontology

Fingerprint

Dive into the research topics of 'Potential for Southern Hemisphere climate surprises'. Together they form a unique fingerprint.

Cite this