Articles | Volume 12, issue 7
Clim. Past, 12, 1435–1444, 2016
https://doi.org/10.5194/cp-12-1435-2016

Special issue: Southern perspectives on climate and the environment from...

Clim. Past, 12, 1435–1444, 2016
https://doi.org/10.5194/cp-12-1435-2016

Research article 05 Jul 2016

Research article | 05 Jul 2016

Constant wind regimes during the Last Glacial Maximum and early Holocene: evidence from Little Llangothlin Lagoon, New England Tablelands, eastern Australia

James Shulmeister et al.

Viewed

Total article views: 1,908 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,105 634 169 1,908 319 79 96
  • HTML: 1,105
  • PDF: 634
  • XML: 169
  • Total: 1,908
  • Supplement: 319
  • BibTeX: 79
  • EndNote: 96
Views and downloads (calculated since 06 Apr 2016)
Cumulative views and downloads (calculated since 06 Apr 2016)

Cited

Saved (preprint)

Discussed (final revised paper)

Latest update: 01 Dec 2021
Download
Short summary
This paper highlights that small dunes (lunettes) formed on the eastern side of a lake in the Australian sub-tropics at the height of the last ice age (about 21,000 years ago) and in the early part of the current interglacial (9–6,000 years ago). This means that it was fairly wet at these times and also that there were strong westerly winds to form the dunes. Today strong westerly winds occur in winter, and we infer that the same was also true at those times, suggesting no change in circulation.