Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau

Polar stratospheric ozone has decreased since the 1970s due to anthropogenic emissions of chlorofluorocarbons and halons, resulting in the formation of an ozone hole over Antarctica. The effects of the ozone hole and the associated increase in incoming UV-radiation on terrestrial and marine ecosyste...

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Main Authors: Spolaor, Andrea, Burgay, François, Fernandez, Rafael Pedro, Turetta, Carla, Cuevas, Carlos A., Kim, Kitae, Kinnison, Douglas E., Lamarque, Jean-Francoise, de Blasi, Fabrizio, Barbaro, Elena, Corella, Juan Pablo, Barbante, Carlo, Saiz López, Alfonso, Vallelonga, Paul, Massimo, Frezzotti
Format: Book
Language:English
Published: Copernicus Publications
Subjects:
Online Access:http://hdl.handle.net/11336/238300
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author Spolaor, Andrea
Burgay, François
Fernandez, Rafael Pedro
Turetta, Carla
Cuevas, Carlos A.
Kim, Kitae
Kinnison, Douglas E.
Lamarque, Jean-Francoise
de Blasi, Fabrizio
Barbaro, Elena
Corella, Juan Pablo
Barbante, Carlo
Saiz López, Alfonso
Vallelonga, Paul
Massimo, Frezzotti
author_facet Spolaor, Andrea
Burgay, François
Fernandez, Rafael Pedro
Turetta, Carla
Cuevas, Carlos A.
Kim, Kitae
Kinnison, Douglas E.
Lamarque, Jean-Francoise
de Blasi, Fabrizio
Barbaro, Elena
Corella, Juan Pablo
Barbante, Carlo
Saiz López, Alfonso
Vallelonga, Paul
Massimo, Frezzotti
author_sort Spolaor, Andrea
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
description Polar stratospheric ozone has decreased since the 1970s due to anthropogenic emissions of chlorofluorocarbons and halons, resulting in the formation of an ozone hole over Antarctica. The effects of the ozone hole and the associated increase in incoming UV-radiation on terrestrial and marine ecosystems are well studied, however the impact on geochemical cycles of ice photoactive elements, such as iodine, remains almost unexplored. Here, we present the first iodine record from the inner Antarctic Plateau (Dome C) that covers approximately the last 212 years (1800-2012 CE). Our results show that iodine concentration in ice remained fairly constant during the pre-ozone hole period (1800-1974 CE) but has declined twofold since the onset of the ozone hole era (~1975 CE), closely tracking the total ozone evolution over Antarctica. Based on ice core observations, laboratory measurements and chemistry-climate model simulations, we propose that the iodine decrease since ~1975 is caused by enhanced iodine re-emission from snowpack due to the ozone hole driven increase in UV-radiation reaching the Antarctic Plateau. These findings suggest the potential for ice core iodine records from the inner Antarctic Plateau as an archive for past stratospheric ozone trends. Fil: Spolaor, Andrea. National Research Council of Italy. Institute of Polar Sciences; Italia. Università Ca’ Foscari di Venezia; Italia Fil: Burgay, François. Università Ca’ Foscari di Venezia; Italia. Paul Scherrer Institut. Laboratory of Environmental Chemistry; 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. Universidad Nacional de Cuyo. Facultad de Ciencias Exactas y Naturales; Argentina Fil: Turetta, Carla. National Research Council of Italy, Institute of Polar Sciences; Italia. Università Ca’ Foscari di Venezia; ...
format Book
genre Antarc*
Antarctic
Antarctica
ice core
genre_facet Antarc*
Antarctic
Antarctica
ice core
geographic Antarctic
Argentina
Fernandez
The Antarctic
geographic_facet Antarctic
Argentina
Fernandez
The Antarctic
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institution Open Polar
language English
long_lat ENVELOPE(-62.233,-62.233,-63.250,-63.250)
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op_doi https://doi.org/10.5194/egusphere-egu22-3777
op_relation info:eu-repo/semantics/altIdentifier/url/https://meetingorganizer.copernicus.org/EGU22/EGU22-3777.html
info:eu-repo/semantics/altIdentifier/url/https://doi.org/10.5194/egusphere-egu22-3777
http://hdl.handle.net/11336/238300
Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau; European Geosciences Union General Assembly
Viena; Austria; 2022
CONICET Digital
CONICET
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publisher Copernicus Publications
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/238300 2025-01-16T19:42:07+00:00 Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau Spolaor, Andrea Burgay, François Fernandez, Rafael Pedro Turetta, Carla Cuevas, Carlos A. Kim, Kitae Kinnison, Douglas E. Lamarque, Jean-Francoise de Blasi, Fabrizio Barbaro, Elena Corella, Juan Pablo Barbante, Carlo Saiz López, Alfonso Vallelonga, Paul Massimo, Frezzotti Internacional application/pdf http://hdl.handle.net/11336/238300 eng eng Copernicus Publications info:eu-repo/semantics/altIdentifier/url/https://meetingorganizer.copernicus.org/EGU22/EGU22-3777.html info:eu-repo/semantics/altIdentifier/url/https://doi.org/10.5194/egusphere-egu22-3777 http://hdl.handle.net/11336/238300 Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau; European Geosciences Union General Assembly Viena; Austria; 2022 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ Iodine geochemistry Ozone hole Dome-C Ice-core halogens https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/conferenceObject info:ar-repo/semantics/documento de conferencia Congreso Book ftconicet https://doi.org/10.5194/egusphere-egu22-3777 2024-10-04T09:34:03Z Polar stratospheric ozone has decreased since the 1970s due to anthropogenic emissions of chlorofluorocarbons and halons, resulting in the formation of an ozone hole over Antarctica. The effects of the ozone hole and the associated increase in incoming UV-radiation on terrestrial and marine ecosystems are well studied, however the impact on geochemical cycles of ice photoactive elements, such as iodine, remains almost unexplored. Here, we present the first iodine record from the inner Antarctic Plateau (Dome C) that covers approximately the last 212 years (1800-2012 CE). Our results show that iodine concentration in ice remained fairly constant during the pre-ozone hole period (1800-1974 CE) but has declined twofold since the onset of the ozone hole era (~1975 CE), closely tracking the total ozone evolution over Antarctica. Based on ice core observations, laboratory measurements and chemistry-climate model simulations, we propose that the iodine decrease since ~1975 is caused by enhanced iodine re-emission from snowpack due to the ozone hole driven increase in UV-radiation reaching the Antarctic Plateau. These findings suggest the potential for ice core iodine records from the inner Antarctic Plateau as an archive for past stratospheric ozone trends. Fil: Spolaor, Andrea. National Research Council of Italy. Institute of Polar Sciences; Italia. Università Ca’ Foscari di Venezia; Italia Fil: Burgay, François. Università Ca’ Foscari di Venezia; Italia. Paul Scherrer Institut. Laboratory of Environmental Chemistry; 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. Universidad Nacional de Cuyo. Facultad de Ciencias Exactas y Naturales; Argentina Fil: Turetta, Carla. National Research Council of Italy, Institute of Polar Sciences; Italia. Università Ca’ Foscari di Venezia; ... Book Antarc* Antarctic Antarctica ice core CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic Argentina Fernandez ENVELOPE(-62.233,-62.233,-63.250,-63.250) The Antarctic
spellingShingle Iodine geochemistry
Ozone hole
Dome-C
Ice-core halogens
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Spolaor, Andrea
Burgay, François
Fernandez, Rafael Pedro
Turetta, Carla
Cuevas, Carlos A.
Kim, Kitae
Kinnison, Douglas E.
Lamarque, Jean-Francoise
de Blasi, Fabrizio
Barbaro, Elena
Corella, Juan Pablo
Barbante, Carlo
Saiz López, Alfonso
Vallelonga, Paul
Massimo, Frezzotti
Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
title Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
title_full Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
title_fullStr Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
title_full_unstemmed Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
title_short Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
title_sort antarctic ozone hole modifies iodine geochemistry on the antarctic plateau
topic Iodine geochemistry
Ozone hole
Dome-C
Ice-core halogens
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Iodine geochemistry
Ozone hole
Dome-C
Ice-core halogens
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/238300