Abstract
Post-depositional processes alter the water stable isotopic signal recorded in the snow and firn. However, the processes involved in the formation of the seasonal cycle in the snow surface remain poorly constrained. It is also uncertain to what extent post-depositional processes influence the mean and variability of the multi-decadal isotopic signal at low accumulation sites. Here we simulate the isotopic signal in the snow surface and in a 30-year (1994–2024) snow core at Dome C in East Antarctica. We argue that mixing new precipitation with the snow in a surface layer needs to be considered through an effective mixing depth. Using an effective mixing depth of 4 cm allows to simulate the observed mean post-depositional alteration of the snow surface. Considering vapor exchange improves the representation of both the observed amplitude of the seasonal cycle and the observed monthly mean variability in the snow surface isotopic signal (δ18O and d-excess) over five years. In addition, we show that vapor exchange leads to a decrease in the δ18O inter-annual variability (−11 %) and an increase in the d-excess inter-annual variability (+33 %) in a 30-year snow core. Our results highlight that (i) isotopic fractionation during surface vapor exchange in combination with mixing at the surface are key drivers of the isotopic signal in the snow surface, (ii) surface vapor exchange alters the mean and variability in multi-decadal isotopic records at Dome C, and (iii) precipitation intermittency modulates the magnitude of the impact of vapor exchange on the snow core isotopic profiles.
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Inès Ollivier, Hans Christian Steen-Larsen, Laura J. Dietrich, et al.
Post-depositional Processes Alter the Seasonal and Multi-decadal Water Isotopic Records in Antarctic Snow and Firn. Authorea. 08 October 2025.
DOI: https://doi.org/10.22541/au.175994561.12898624/v1
DOI: https://doi.org/10.22541/au.175994561.12898624/v1
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