Challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from Adélie Land, coastal Antarctica
A new 21.3 m firn core was drilled in 2015 at a coastal Antarctic high-accumulation site in Adélie Land (66.78 ∘ S; 139.56 ∘ E, 602 m a.s.l.), named Terre Adélie 192A (TA192A). The mean isotopic values ( <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="in...
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ftcopernicus:oai:publications.copernicus.org:tc69698 2023-05-15T13:55:28+02:00 Challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from Adélie Land, coastal Antarctica Goursaud, Sentia Masson-Delmotte, Valérie Favier, Vincent Preunkert, Suzanne Legrand, Michel Minster, Bénédicte Werner, Martin 2019-04-24 application/pdf https://doi.org/10.5194/tc-13-1297-2019 https://tc.copernicus.org/articles/13/1297/2019/ eng eng doi:10.5194/tc-13-1297-2019 https://tc.copernicus.org/articles/13/1297/2019/ eISSN: 1994-0424 Text 2019 ftcopernicus https://doi.org/10.5194/tc-13-1297-2019 2020-07-20T16:22:51Z A new 21.3 m firn core was drilled in 2015 at a coastal Antarctic high-accumulation site in Adélie Land (66.78 ∘ S; 139.56 ∘ E, 602 m a.s.l.), named Terre Adélie 192A (TA192A). The mean isotopic values ( <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">19.3</mn><mspace width="0.125em" linebreak="nobreak"/><mi mathvariant="normal">‰</mi><mo>±</mo><mn mathvariant="normal">3.1</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="70pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="8c7cb92ef210551f462adaf6959f644a"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-13-1297-2019-ie00001.svg" width="70pt" height="10pt" src="tc-13-1297-2019-ie00001.png"/></svg:svg> ‰ for δ 18 O and 5.4 ‰±2.2 ‰ for deuterium excess) are consistent with other coastal Antarctic values. No significant isotope–temperature relationship can be evidenced at any timescale. This rules out a simple interpretation in terms of local temperature. An observed asymmetry in the δ 18 O seasonal cycle may be explained by the precipitation of air masses coming from the eastern and western sectors in autumn and winter, recorded in the d -excess signal showing outstanding values in austral spring versus autumn. Significant positive trends are observed in the annual d -excess record and local sea ice extent (135–145 ∘ E) over the period 1998–2014. However, process studies focusing on resulting isotopic compositions and particularly the deuterium excess– δ 18 O relationship, evidenced as a potential fingerprint of moisture origins, as well as the collection of more isotopic measurements in Adélie Land are needed for an accurate interpretation of our signals. Text Antarc* Antarctic Antarctica Sea ice Copernicus Publications: E-Journals Antarctic Austral Terre Adélie ENVELOPE(139.000,139.000,-67.000,-67.000) Terre-Adélie ENVELOPE(138.991,138.991,-59.999,-59.999) The Cryosphere 13 4 1297 1324 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
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English |
description |
A new 21.3 m firn core was drilled in 2015 at a coastal Antarctic high-accumulation site in Adélie Land (66.78 ∘ S; 139.56 ∘ E, 602 m a.s.l.), named Terre Adélie 192A (TA192A). The mean isotopic values ( <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">19.3</mn><mspace width="0.125em" linebreak="nobreak"/><mi mathvariant="normal">‰</mi><mo>±</mo><mn mathvariant="normal">3.1</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="70pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="8c7cb92ef210551f462adaf6959f644a"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-13-1297-2019-ie00001.svg" width="70pt" height="10pt" src="tc-13-1297-2019-ie00001.png"/></svg:svg> ‰ for δ 18 O and 5.4 ‰±2.2 ‰ for deuterium excess) are consistent with other coastal Antarctic values. No significant isotope–temperature relationship can be evidenced at any timescale. This rules out a simple interpretation in terms of local temperature. An observed asymmetry in the δ 18 O seasonal cycle may be explained by the precipitation of air masses coming from the eastern and western sectors in autumn and winter, recorded in the d -excess signal showing outstanding values in austral spring versus autumn. Significant positive trends are observed in the annual d -excess record and local sea ice extent (135–145 ∘ E) over the period 1998–2014. However, process studies focusing on resulting isotopic compositions and particularly the deuterium excess– δ 18 O relationship, evidenced as a potential fingerprint of moisture origins, as well as the collection of more isotopic measurements in Adélie Land are needed for an accurate interpretation of our signals. |
format |
Text |
author |
Goursaud, Sentia Masson-Delmotte, Valérie Favier, Vincent Preunkert, Suzanne Legrand, Michel Minster, Bénédicte Werner, Martin |
spellingShingle |
Goursaud, Sentia Masson-Delmotte, Valérie Favier, Vincent Preunkert, Suzanne Legrand, Michel Minster, Bénédicte Werner, Martin Challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from Adélie Land, coastal Antarctica |
author_facet |
Goursaud, Sentia Masson-Delmotte, Valérie Favier, Vincent Preunkert, Suzanne Legrand, Michel Minster, Bénédicte Werner, Martin |
author_sort |
Goursaud, Sentia |
title |
Challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from Adélie Land, coastal Antarctica |
title_short |
Challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from Adélie Land, coastal Antarctica |
title_full |
Challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from Adélie Land, coastal Antarctica |
title_fullStr |
Challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from Adélie Land, coastal Antarctica |
title_full_unstemmed |
Challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from Adélie Land, coastal Antarctica |
title_sort |
challenges associated with the climatic interpretation of water stable isotope records from a highly resolved firn core from adélie land, coastal antarctica |
publishDate |
2019 |
url |
https://doi.org/10.5194/tc-13-1297-2019 https://tc.copernicus.org/articles/13/1297/2019/ |
long_lat |
ENVELOPE(139.000,139.000,-67.000,-67.000) ENVELOPE(138.991,138.991,-59.999,-59.999) |
geographic |
Antarctic Austral Terre Adélie Terre-Adélie |
geographic_facet |
Antarctic Austral Terre Adélie Terre-Adélie |
genre |
Antarc* Antarctic Antarctica Sea ice |
genre_facet |
Antarc* Antarctic Antarctica Sea ice |
op_source |
eISSN: 1994-0424 |
op_relation |
doi:10.5194/tc-13-1297-2019 https://tc.copernicus.org/articles/13/1297/2019/ |
op_doi |
https://doi.org/10.5194/tc-13-1297-2019 |
container_title |
The Cryosphere |
container_volume |
13 |
container_issue |
4 |
container_start_page |
1297 |
op_container_end_page |
1324 |
_version_ |
1766262115074572288 |