Surface snow triple isotopic composition at Dome C, Antarctica

Water isotope ratios of ice cores are a key source of information on past temperatures. Throughout the hydrological cycle, temperature is imprinted in the water isotopic composition of snowfalls. However, this signal of climatic interest is modified after deposition when snow remains at the surface...

Full description

Bibliographic Details
Main Authors: Casado, Mathieu, Landais, Amaelle, Picard, Ghislain, Arnaud, Laurent, Dreossi, Giuliano, Stenni, Barbara, Prié, Frédéric
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2021
Subjects:
Antarctica
excess
metamorphism
surface snow
water isotopes
Quantitative picture of interactions between climate, hydrological cycle and stratospheric inputs in Antarctica over the last 100 years via the combined use of all water isotopes COMBINISO
Antarc*
ice core
Online Access:https://dx.doi.org/10.1594/pangaea.934273
https://doi.pangaea.de/10.1594/PANGAEA.934273
Description
Summary:Water isotope ratios of ice cores are a key source of information on past temperatures. Throughout the hydrological cycle, temperature is imprinted in the water isotopic composition of snowfalls. However, this signal of climatic interest is modified after deposition when snow remains at the surface exposed to the atmosphere. Comparing time series of surface snow isotopic composition at Dome C with satellite observations of surface snow metamorphism, we found that long summer periods without precipitation favour surface snow metamorphism altering the surface snow isotopic composition. Using excess parameters (combining D,17O, and 18O fractions) allow the identification of this alteration caused by sublimation and condensation of surface hoar. The combined measurement of all three isotopic compositions could help identifying ice core sections influenced by snow metamorphism in sites with very low snow accumulation.

Similar Items