Articles | Volume 13, issue 10
https://doi.org/10.5194/cp-13-1301-2017
https://doi.org/10.5194/cp-13-1301-2017
Research article
 | 
04 Oct 2017
Research article |  | 04 Oct 2017

Late Holocene intensification of the westerly winds at the subantarctic Auckland Islands (51° S), New Zealand

Imogen M. Browne, Christopher M. Moy, Christina R. Riesselman, Helen L. Neil, Lorelei G. Curtin, Andrew R. Gorman, and Gary S. Wilson

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ED: Publish subject to minor revisions (review by Editor) (04 Jul 2017) by Maisa Rojas
AR by Imogen Browne on behalf of the Authors (17 Jul 2017)  Author's response   Manuscript 
ED: Publish subject to technical corrections (01 Aug 2017) by Maisa Rojas
AR by Imogen Browne on behalf of the Authors (04 Aug 2017)  Author's response   Manuscript 
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Short summary
The westerly winds determine weather patterns and exert an effect on carbon dioxide (CO2) flux in and out of the Southern Ocean, an important sink for atmospheric CO2. Our research reconstructs changes in the westerlies over the past 5000 years, using a marine sediment core record collected from the subantarctic Auckland Islands. Our results indicate an intensification of the westerlies around 1600 years ago, contemporaneous with other records from comparable latitudes across the Pacific Ocean.