Barbara Stenni

Abstract Water isotopes serve as tracers of hydrological processes and as proxies for past climates archived in ice cores. The isotopic signal is acquired throughout the hydrological cycle—through evaporation over the oceans, precipitation, which occurs as moisture is transported from lower to higher latitudes, and during post-depositional processes in which isotopic exchange between snow and atmospheric moisture occurs.

Article Dans Une Revue The Holocene Année : 2016 Common millennial-scale variability of Antarctic and Southern Ocean temperatures during the past 5000 years reconstructed from the EPICA Dome C ice core Origine Fichiers produits par l'(les) auteur(s) hal-03102630 , version 1 (23-04-2025) Valérie Masson-Delmotte, Barbara Stenni, Jean Jouzel. Common millennial-scale variability of Antarctic and Southern Ocean temperatures during the past 5000 years reconstructed from the EPICA Dome C ice core.

Correction to: Nature Communications https://doi.org/10.1038/s41467-022-32847-3, published online 10 September 2022 The original version of this Article contained formatting errors in Table 1. The time interval was reported as 11–127 ka, this has been corrected to 117–127 ka. The column labels and data were incorrectly aligned. This has been corrected in both the PDF and HTML versions of the Article.