Articles | Volume 14, issue 12
https://doi.org/10.5194/cp-14-2053-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-14-2053-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
What climate signal is contained in decadal- to centennial-scale isotope variations from Antarctic ice cores?
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und
Meeresforschung, Research Unit Potsdam, Telegrafenberg A45, 14473 Potsdam,
Germany
University of Potsdam, Institute of Physics and Astronomy,
Karl-Liebknecht-Str. 24/25, 14476 Potsdam, Germany
Thomas Laepple
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und
Meeresforschung, Research Unit Potsdam, Telegrafenberg A45, 14473 Potsdam,
Germany
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- Deciphering stable water isotope records of firn cores from a strongly maritime, high-accumulation site on the Antarctic Peninsula K. Hoffmann-Abdi et al. 10.1017/jog.2023.79
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- The role of sublimation as a driver of climate signals in the water isotope content of surface snow: laboratory and field experimental results A. Hughes et al. 10.5194/tc-15-4949-2021
- A decade (2008–2017) of water stable isotope composition of precipitation at Concordia Station, East Antarctica G. Dreossi et al. 10.5194/tc-18-3911-2024
- A Snapshot on the Buildup of the Stable Water Isotopic Signal in the Upper Snowpack at EastGRIP on the Greenland Ice Sheet A. Zuhr et al. 10.1029/2022JF006767
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- Climatic information archived in ice cores: impact of intermittency and diffusion on the recorded isotopic signal in Antarctica M. Casado et al. 10.5194/cp-16-1581-2020
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- Microstructure of Snow and Its Link to Trace Elements and Isotopic Composition at Kohnen Station, Dronning Maud Land, Antarctica D. Moser et al. 10.3389/feart.2020.00023
- A spectral approach to estimating the timescale-dependent uncertainty of paleoclimate records – Part 1: Theoretical concept T. Kunz et al. 10.5194/cp-16-1469-2020
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- Spatial variability and post-depositional diffusion of stable isotopes in high accumulation regions of East Antarctica K. Mahalinganathan et al. 10.3389/feart.2022.925447
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- From atmospheric water isotopes measurement to firn core interpretation in Adélie Land: a case study for isotope-enabled atmospheric models in Antarctica C. Leroy-Dos Santos et al. 10.5194/tc-17-5241-2023
- The Structure of Climate Variability Across Scales C. Franzke et al. 10.1029/2019RG000657
- Stratigraphic noise and its potential drivers across the plateau of Dronning Maud Land, East Antarctica N. Hirsch et al. 10.5194/tc-17-4207-2023
- Water Isotopic Signature of Surface Snow Metamorphism in Antarctica M. Casado et al. 10.1029/2021GL093382
- Modern temperatures in central–north Greenland warmest in past millennium M. Hörhold et al. 10.1038/s41586-022-05517-z
- Empirical estimate of the signal content of Holocene temperature proxy records M. Reschke et al. 10.5194/cp-15-521-2019
- Resonant Forcing of the Climate System in Subharmonic Modes J. Pinault 10.3390/jmse8010060
- Climatology of the Mount Brown South ice core site in East Antarctica: implications for the interpretation of a water isotope record S. Jackson et al. 10.5194/cp-19-1653-2023
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- Stable water isotopes and accumulation rates in the Union Glacier region, Ellsworth Mountains, West Antarctica, over the last 35 years K. Hoffmann et al. 10.5194/tc-14-881-2020
- A 2000-year temperature reconstruction on the East Antarctic plateau from argon–nitrogen and water stable isotopes in the Aurora Basin North ice core A. Servettaz et al. 10.5194/cp-19-1125-2023
- The quandary of detecting the signature of climate change in Antarctica M. Casado et al. 10.1038/s41558-023-01791-5
Latest update: 05 Dec 2024
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.
Proxy data on climate variations contain noise from many sources and, for reliable estimates, we...