Articles | Volume 12, issue 7
https://doi.org/10.5194/cp-12-1565-2016
https://doi.org/10.5194/cp-12-1565-2016
Research article
 | 
22 Jul 2016
Research article |  | 22 Jul 2016

Regional climate signal vs. local noise: a two-dimensional view of water isotopes in Antarctic firn at Kohnen Station, Dronning Maud Land

Thomas Münch, Sepp Kipfstuhl, Johannes Freitag, Hanno Meyer, and Thomas Laepple

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (22 Feb 2016) by Eric Wolff
AR by Thomas Münch on behalf of the Authors (04 Apr 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (14 Apr 2016) by Eric Wolff
RR by Anonymous Referee #2 (09 May 2016)
RR by Anonymous Referee #1 (18 May 2016)
ED: Publish subject to minor revisions (review by Editor) (27 May 2016) by Eric Wolff
AR by Thomas Münch on behalf of the Authors (13 Jun 2016)  Author's response   Manuscript 
ED: Publish as is (14 Jun 2016) by Eric Wolff
AR by Thomas Münch on behalf of the Authors (22 Jun 2016)
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Short summary
Ice-core oxygen isotope ratios are a key climate archive to infer past temperatures, an interpretation however complicated by non-climatic noise. Based on 50 m firn trenches, we present for the first time a two-dimensional view (vertical × horizontal) of how oxygen isotopes are stored in Antarctic firn. A statistical noise model allows inferences for the validity of ice coring efforts to reconstruct past temperatures, highlighting the need of replicate cores for Holocene climate reconstructions.