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...
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ftdatacite:10.1594/pangaea.934273 2024-09-15T17:42:28+00:00 Surface snow triple isotopic composition at Dome C, Antarctica ... Casado, Mathieu Landais, Amaëlle Picard, Ghislain Arnaud, Laurent Dreossi, Giuliano Stenni, Barbara Prié, Frédéric 2021 application/zip https://dx.doi.org/10.1594/pangaea.934273 https://doi.pangaea.de/10.1594/PANGAEA.934273 en eng PANGAEA https://dx.doi.org/10.1029/2021gl093382 https://dx.doi.org/10.5194/tc-12-1745-2018 https://dx.doi.org/10.1016/j.rse.2017.07.035 https://dx.doi.org/10.1038/nclimate1590 https://dx.doi.org/10.5194/tc-10-2415-2016 https://dx.doi.org/10.5194/tc-10-837-2016 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 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 article Collection Bundled Publication of Datasets 2021 ftdatacite https://doi.org/10.1594/pangaea.93427310.1029/2021gl09338210.5194/tc-12-1745-201810.1016/j.rse.2017.07.03510.1038/nclimate159010.5194/tc-10-2415-201610.5194/tc-10-837-2016 2024-08-01T10:53:32Z 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. ... Article in Journal/Newspaper Antarc* Antarctica ice core DataCite |
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ftdatacite |
language |
English |
topic |
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 |
spellingShingle |
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 Casado, Mathieu Landais, Amaëlle Picard, Ghislain Arnaud, Laurent Dreossi, Giuliano Stenni, Barbara Prié, Frédéric Surface snow triple isotopic composition at Dome C, Antarctica ... |
topic_facet |
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 |
description |
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 |
Article in Journal/Newspaper |
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 |
author_sort |
Casado, Mathieu |
title |
Surface snow triple isotopic composition at Dome C, Antarctica ... |
title_short |
Surface snow triple isotopic composition at Dome C, Antarctica ... |
title_full |
Surface snow triple isotopic composition at Dome C, Antarctica ... |
title_fullStr |
Surface snow triple isotopic composition at Dome C, Antarctica ... |
title_full_unstemmed |
Surface snow triple isotopic composition at Dome C, Antarctica ... |
title_sort |
surface snow triple isotopic composition at dome c, antarctica ... |
publisher |
PANGAEA |
publishDate |
2021 |
url |
https://dx.doi.org/10.1594/pangaea.934273 https://doi.pangaea.de/10.1594/PANGAEA.934273 |
genre |
Antarc* Antarctica ice core |
genre_facet |
Antarc* Antarctica ice core |
op_relation |
https://dx.doi.org/10.1029/2021gl093382 https://dx.doi.org/10.5194/tc-12-1745-2018 https://dx.doi.org/10.1016/j.rse.2017.07.035 https://dx.doi.org/10.1038/nclimate1590 https://dx.doi.org/10.5194/tc-10-2415-2016 https://dx.doi.org/10.5194/tc-10-837-2016 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.93427310.1029/2021gl09338210.5194/tc-12-1745-201810.1016/j.rse.2017.07.03510.1038/nclimate159010.5194/tc-10-2415-201610.5194/tc-10-837-2016 |
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1810489048894013440 |