200-year ice core bromine reconstruction at Dome C (Antarctica): Observational and modelling results
Bromine enrichment (Brenr) has been proposed as an ice core proxy for past sea-ice reconstruction. Understanding the processes that influence bromine preservation in the ice is crucial to achieve a reliable interpretation of ice core signals and to potentially relate them to past sea-ice variability...
Published in: | The Cryosphere |
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Main Authors: | , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
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Online Access: | http://hdl.handle.net/11336/219092 |
_version_ | 1821776948002553856 |
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author | Burgay, François Fernandez, Rafael Pedro Segato, Delia Turetta, Clara Blaszczak Boxe, Christopher S. Rhodes, Rachael H. Scarchilli, Claudio Ciardini, Virginia Barbante, Carlo Saiz López, Alfonso Spolaor, Andrea |
author_facet | Burgay, François Fernandez, Rafael Pedro Segato, Delia Turetta, Clara Blaszczak Boxe, Christopher S. Rhodes, Rachael H. Scarchilli, Claudio Ciardini, Virginia Barbante, Carlo Saiz López, Alfonso Spolaor, Andrea |
author_sort | Burgay, François |
collection | CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
container_issue | 1 |
container_start_page | 391 |
container_title | The Cryosphere |
container_volume | 17 |
description | Bromine enrichment (Brenr) has been proposed as an ice core proxy for past sea-ice reconstruction. Understanding the processes that influence bromine preservation in the ice is crucial to achieve a reliable interpretation of ice core signals and to potentially relate them to past sea-ice variability. Here, we present a 210 years bromine record that sheds light on the main processes controlling bromine preservation in the snow and ice at Dome C, East Antarctic plateau. Using observations alongside a modelling approach, we demonstrate that the bromine signal is preserved at Dome C and it is not affected by the strong variations in ultraviolet radiation reaching the Antarctic plateau due to the stratospheric ozone hole. Based on this, we investigate whether the Dome C Brenr record can be used as an effective tracer of past Antarctic sea ice. Due to the limited time window covered by satellite measurements and the low sea-ice variability observed during the last 30 years in East Antarctica, we cannot fully validate Brenr as an effective proxy for past sea-ice reconstructions at Dome C. Fil: Burgay, François. Universita' Ca' Foscari Di Venezia; Italia. Paul Scherrer Institut; Suiza Fil: Fernandez, Rafael Pedro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Básicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Básicas; Argentina Fil: Segato, Delia. Consiglio Nazionale delle Ricerche; Italia. Universita' Ca' Foscari Di Venezia; Italia Fil: Turetta, Clara. Consiglio Nazionale delle Ricerche; Italia. Universita' Ca' Foscari Di Venezia; Italia Fil: Blaszczak Boxe, Christopher S. Howard University; Estados Unidos Fil: Rhodes, Rachael H. University of Cambridge; Estados Unidos Fil: Scarchilli, Claudio. Laboratory of Observations And Measures for the Environment and Climate; Italia Fil: Ciardini, Virginia. Laboratory of Observations And Measures for the Environment and Climate; ... |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctic Antarctica East Antarctica ice core Sea ice |
genre_facet | Antarc* Antarctic Antarctica East Antarctica ice core Sea ice |
geographic | Antarctic Argentina East Antarctica Fernandez The Antarctic |
geographic_facet | Antarctic Argentina East Antarctica Fernandez The Antarctic |
id | ftconicet:oai:ri.conicet.gov.ar:11336/219092 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-62.233,-62.233,-63.250,-63.250) |
op_collection_id | ftconicet |
op_container_end_page | 405 |
op_doi | https://doi.org/10.5194/tc-17-391-2023 |
op_relation | info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-17-391-2023 info:eu-repo/semantics/altIdentifier/url/https://tc.copernicus.org/articles/17/391/2023/ http://hdl.handle.net/11336/219092 CONICET Digital CONICET |
op_rights | info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ |
publisher | Copernicus Publications |
record_format | openpolar |
spelling | ftconicet:oai:ri.conicet.gov.ar:11336/219092 2025-01-16T19:42:20+00:00 200-year ice core bromine reconstruction at Dome C (Antarctica): Observational and modelling results Burgay, François Fernandez, Rafael Pedro Segato, Delia Turetta, Clara Blaszczak Boxe, Christopher S. Rhodes, Rachael H. Scarchilli, Claudio Ciardini, Virginia Barbante, Carlo Saiz López, Alfonso Spolaor, Andrea application/pdf http://hdl.handle.net/11336/219092 eng eng Copernicus Publications info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-17-391-2023 info:eu-repo/semantics/altIdentifier/url/https://tc.copernicus.org/articles/17/391/2023/ http://hdl.handle.net/11336/219092 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ Dome-C Antarctica eSa-ice Bromine Ice-core halogens https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.5194/tc-17-391-2023 2024-10-04T09:34:18Z Bromine enrichment (Brenr) has been proposed as an ice core proxy for past sea-ice reconstruction. Understanding the processes that influence bromine preservation in the ice is crucial to achieve a reliable interpretation of ice core signals and to potentially relate them to past sea-ice variability. Here, we present a 210 years bromine record that sheds light on the main processes controlling bromine preservation in the snow and ice at Dome C, East Antarctic plateau. Using observations alongside a modelling approach, we demonstrate that the bromine signal is preserved at Dome C and it is not affected by the strong variations in ultraviolet radiation reaching the Antarctic plateau due to the stratospheric ozone hole. Based on this, we investigate whether the Dome C Brenr record can be used as an effective tracer of past Antarctic sea ice. Due to the limited time window covered by satellite measurements and the low sea-ice variability observed during the last 30 years in East Antarctica, we cannot fully validate Brenr as an effective proxy for past sea-ice reconstructions at Dome C. Fil: Burgay, François. Universita' Ca' Foscari Di Venezia; Italia. Paul Scherrer Institut; Suiza Fil: Fernandez, Rafael Pedro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Interdisciplinario de Ciencias Básicas. - Universidad Nacional de Cuyo. Instituto Interdisciplinario de Ciencias Básicas; Argentina Fil: Segato, Delia. Consiglio Nazionale delle Ricerche; Italia. Universita' Ca' Foscari Di Venezia; Italia Fil: Turetta, Clara. Consiglio Nazionale delle Ricerche; Italia. Universita' Ca' Foscari Di Venezia; Italia Fil: Blaszczak Boxe, Christopher S. Howard University; Estados Unidos Fil: Rhodes, Rachael H. University of Cambridge; Estados Unidos Fil: Scarchilli, Claudio. Laboratory of Observations And Measures for the Environment and Climate; Italia Fil: Ciardini, Virginia. Laboratory of Observations And Measures for the Environment and Climate; ... Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica ice core Sea ice CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic Argentina East Antarctica Fernandez ENVELOPE(-62.233,-62.233,-63.250,-63.250) The Antarctic The Cryosphere 17 1 391 405 |
spellingShingle | Dome-C Antarctica eSa-ice Bromine Ice-core halogens https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Burgay, François Fernandez, Rafael Pedro Segato, Delia Turetta, Clara Blaszczak Boxe, Christopher S. Rhodes, Rachael H. Scarchilli, Claudio Ciardini, Virginia Barbante, Carlo Saiz López, Alfonso Spolaor, Andrea 200-year ice core bromine reconstruction at Dome C (Antarctica): Observational and modelling results |
title | 200-year ice core bromine reconstruction at Dome C (Antarctica): Observational and modelling results |
title_full | 200-year ice core bromine reconstruction at Dome C (Antarctica): Observational and modelling results |
title_fullStr | 200-year ice core bromine reconstruction at Dome C (Antarctica): Observational and modelling results |
title_full_unstemmed | 200-year ice core bromine reconstruction at Dome C (Antarctica): Observational and modelling results |
title_short | 200-year ice core bromine reconstruction at Dome C (Antarctica): Observational and modelling results |
title_sort | 200-year ice core bromine reconstruction at dome c (antarctica): observational and modelling results |
topic | Dome-C Antarctica eSa-ice Bromine Ice-core halogens https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
topic_facet | Dome-C Antarctica eSa-ice Bromine Ice-core halogens https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
url | http://hdl.handle.net/11336/219092 |