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

In low-accumulation regions, the reliability of δ 18 O-derived temperature signals from ice cores within the Holocene is unclear, primarily due to the small climate changes relative to the intrinsic noise of the isotopic signal. In order to learn about the representativity of single ice cores and to...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: T. Münch, S. Kipfstuhl, J. Freitag, H. Meyer, T. Laepple
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2016
Subjects:
Online Access:https://doi.org/10.5194/cp-12-1565-2016
https://doaj.org/article/61fcab4ecec7476dae0f72993a71183d