Stable water-isotope records from Antarctic ice cores allow the reconstruction of past temperature variability. However, accurate interpretation of the isotopic signal requires comprehensive understanding of the processes leading to its archiving in snow and ice, which can be documented by in situ measurements.

From precipitation to ice core: On the importance of surface processes for stable water-isotope records in East Antarctica

Barbara Stenni;
2023-01-01

Abstract

Stable water-isotope records from Antarctic ice cores allow the reconstruction of past temperature variability. However, accurate interpretation of the isotopic signal requires comprehensive understanding of the processes leading to its archiving in snow and ice, which can be documented by in situ measurements.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/10278/5045947
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