Articles | Volume 14, issue 12
https://doi.org/10.5194/cp-14-2053-2018
https://doi.org/10.5194/cp-14-2053-2018
Research article
 | Highlight paper
 | 
20 Dec 2018
Research article | Highlight paper |  | 20 Dec 2018

What climate signal is contained in decadal- to centennial-scale isotope variations from Antarctic ice cores?

Thomas Münch and Thomas Laepple

Viewed

Total article views: 6,757 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
5,426 1,173 158 6,757 107 120
  • HTML: 5,426
  • PDF: 1,173
  • XML: 158
  • Total: 6,757
  • BibTeX: 107
  • EndNote: 120
Views and downloads (calculated since 27 Aug 2018)
Cumulative views and downloads (calculated since 27 Aug 2018)

Viewed (geographical distribution)

Total article views: 6,757 (including HTML, PDF, and XML) Thereof 5,704 with geography defined and 1,053 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 05 Dec 2024
Download
Short summary
Proxy data on climate variations contain noise from many sources and, for reliable estimates, we need to determine those temporal scales at which the climate signal in the proxy record dominates the noise. We developed a method to derive timescale-dependent estimates of temperature proxy signal-to-noise ratios, which we apply and discuss in the context of Antarctic ice-core records but which in general are applicable to a large set of palaeoclimate records.