| _version_ | 1867169518883700736 |
|---|---|
| author | Casado, Mathieu Landais, Amaëlle Picard, Ghislain Arnaud, Laurent Dreossi, Giuliano Stenni, Barbara Prié, Frédéric |
| author_facet | Casado, Mathieu Landais, Amaëlle Picard, Ghislain Arnaud, Laurent Dreossi, Giuliano Stenni, Barbara Prié, Frédéric |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | 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. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_934273 |
| institution | PANGAEA |
| language | en |
| publishDate | 2021 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Surface snow triple isotopic composition at Dome C, Antarctica Casado, Mathieu Landais, Amaëlle Picard, Ghislain Arnaud, Laurent Dreossi, Giuliano Stenni, Barbara Prié, Frédéric Antarctica; COMBINISO; excess; metamorphism; 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; surface snow; water isotopes 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. |
| title | Surface snow triple isotopic composition at Dome C, Antarctica |
| topic | Antarctica; COMBINISO; excess; metamorphism; 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; surface snow; water isotopes |
| url | https://doi.org/10.1594/PANGAEA.934273 |