Oxygen isotopes from two snow trenches from Kohnen Station, Dronning Maud Land, Antarctica from the 2012/13 field season

In low-accumulation regions, the reliability of d18O-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 o...

Full description

Bibliographic Details
Main Authors: Münch, Thomas, Kipfstuhl, Sepp, Freitag, Johannes, Meyer, Hanno, Laepple, Thomas
Format: Dataset
Language:English
Published: PANGAEA 2016
Subjects:
Dronning Maud Land
Kohnen
Kohnen Station
Antarc*
Antarctica
ice core
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.861675
https://doi.org/10.1594/PANGAEA.861675

Similar Items