Articles | Volume 22, issue 9
https://doi.org/10.5194/cp-22-1741-2026
https://doi.org/10.5194/cp-22-1741-2026
Research article
 | 
28 Sep 2026
Research article |  | 28 Sep 2026

Trends in south pole particle concentrations imply holocene westerly wind strengthening

Aaron Chesler, Dominic Winski, Karl Kreutz, Bess Koffman, Erich Osterberg, David Ferris, Zayta Thundercloud, Jihong Cole-Dai, Mark Wells, Aaron Putnam, and Katherine Anderson

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Cited articles

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Aarons, S. M., Aciego, S. M., McConnell, J. R., Delmonte, B., and Baccolo, G.: Dust Transport to the Taylor Glacier, Antarctica, During the Last Interglacial, Geophys. Res. Lett., 46, 2261–2270, https://doi.org/10.1029/2018GL081887, 2019. 
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Albani, S., Delmonte, B., Maggi, V., Baroni, C., Petit, J.-R., Stenni, B., Mazzola, C., and Frezzotti, M.: Interpreting last glacial to Holocene dust changes at Talos Dome (East Antarctica): implications for atmospheric variations from regional to hemispheric scales, Clim. Past, 8, 741–750, https://doi.org/10.5194/cp-8-741-2012, 2012. 
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The Southern Hemisphere Westerly Winds impact global climate and Antarctic ice sheet stability; however, there are few complete records over the past 12 000 years. We use a new mineral dust record from a South Pole ice core and identify a decrease in particle concentration and an increase in coarse particle percentage over the past ~ 11 000 years. Together with other records, our data suggests a southward shift in the winds starting ~ 6500 years ago related to warming in the Southern Hemisphere.
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