Photolytic modification of seasonal nitrate isotope cycles in East Antarctica

<p>Nitrate in Antarctic snow has seasonal cycles in nitrogen and oxygen isotopic ratios that reflect its sources and atmospheric formation processes, and as a result, nitrate archived in Antarctic ice should have great potential to record atmospheric chemistry changes over thousands of years....

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Main Authors: P. D. Akers, J. Savarino, N. Caillon, O. Magand, E. Le Meur
Format: Article
Language:English
Published: Copernicus Publications 2022-12-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/22/15637/2022/acp-22-15637-2022.pdf
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author P. D. Akers
P. D. Akers
J. Savarino
N. Caillon
O. Magand
E. Le Meur
author_facet P. D. Akers
P. D. Akers
J. Savarino
N. Caillon
O. Magand
E. Le Meur
author_sort P. D. Akers
collection DOAJ
description <p>Nitrate in Antarctic snow has seasonal cycles in nitrogen and oxygen isotopic ratios that reflect its sources and atmospheric formation processes, and as a result, nitrate archived in Antarctic ice should have great potential to record atmospheric chemistry changes over thousands of years. However, sunlight that strikes the snow surface results in photolytic nitrate loss and isotopic fractionation that can completely obscure the nitrate's original isotopic values. To gain insight into how photolysis overwrites the seasonal atmospheric cycles, we collected 244 snow samples along an 850 km transect of East Antarctica during the 2013–2014 CHICTABA traverse. The CHICTABA route's limited elevation change, consistent distance between the coast and the high interior plateau, and intermediate accumulation rates offered a gentle environmental gradient ideal for studying the competing pre- and post-depositional influences on archived nitrate isotopes. We find that nitrate isotopes in snow along the transect are indeed notably modified by photolysis after deposition, and drier sites have more intense photolytic impacts. Still, an imprint of the original seasonal cycles of atmospheric nitrate isotopes is present in the top 1–2 <span class="inline-formula">m</span> of the snowpack and likely preserved through archiving in glacial ice at these sites. Despite this preservation, reconstructing past atmospheric values from archived nitrate in similar transitional regions will remain a difficult challenge without having an independent proxy for photolytic loss to correct for post-depositional isotopic changes. Nevertheless, nitrate isotopes should function as a proxy for snow accumulation rate in such regions if multiple years of deposition are aggregated to remove the seasonal cycles, and this application can prove highly valuable in its own right.</p>
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spelling doaj.art-77b886776bbf472ea3d3231506aea9f62022-12-22T04:23:25ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242022-12-0122156371565710.5194/acp-22-15637-2022Photolytic modification of seasonal nitrate isotope cycles in East AntarcticaP. D. Akers0P. D. Akers1J. Savarino2N. Caillon3O. Magand4E. Le Meur5Discipline of Geography, School of Natural Sciences, Trinity College Dublin, Dublin, IrelandUniversité Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, Grenoble, FranceUniversité Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, Grenoble, FranceUniversité Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, Grenoble, FranceUniversité Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, Grenoble, FranceUniversité Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, Grenoble, France<p>Nitrate in Antarctic snow has seasonal cycles in nitrogen and oxygen isotopic ratios that reflect its sources and atmospheric formation processes, and as a result, nitrate archived in Antarctic ice should have great potential to record atmospheric chemistry changes over thousands of years. However, sunlight that strikes the snow surface results in photolytic nitrate loss and isotopic fractionation that can completely obscure the nitrate's original isotopic values. To gain insight into how photolysis overwrites the seasonal atmospheric cycles, we collected 244 snow samples along an 850 km transect of East Antarctica during the 2013–2014 CHICTABA traverse. The CHICTABA route's limited elevation change, consistent distance between the coast and the high interior plateau, and intermediate accumulation rates offered a gentle environmental gradient ideal for studying the competing pre- and post-depositional influences on archived nitrate isotopes. We find that nitrate isotopes in snow along the transect are indeed notably modified by photolysis after deposition, and drier sites have more intense photolytic impacts. Still, an imprint of the original seasonal cycles of atmospheric nitrate isotopes is present in the top 1–2 <span class="inline-formula">m</span> of the snowpack and likely preserved through archiving in glacial ice at these sites. Despite this preservation, reconstructing past atmospheric values from archived nitrate in similar transitional regions will remain a difficult challenge without having an independent proxy for photolytic loss to correct for post-depositional isotopic changes. Nevertheless, nitrate isotopes should function as a proxy for snow accumulation rate in such regions if multiple years of deposition are aggregated to remove the seasonal cycles, and this application can prove highly valuable in its own right.</p>https://acp.copernicus.org/articles/22/15637/2022/acp-22-15637-2022.pdf
spellingShingle P. D. Akers
P. D. Akers
J. Savarino
N. Caillon
O. Magand
E. Le Meur
Photolytic modification of seasonal nitrate isotope cycles in East Antarctica
Atmospheric Chemistry and Physics
title Photolytic modification of seasonal nitrate isotope cycles in East Antarctica
title_full Photolytic modification of seasonal nitrate isotope cycles in East Antarctica
title_fullStr Photolytic modification of seasonal nitrate isotope cycles in East Antarctica
title_full_unstemmed Photolytic modification of seasonal nitrate isotope cycles in East Antarctica
title_short Photolytic modification of seasonal nitrate isotope cycles in East Antarctica
title_sort photolytic modification of seasonal nitrate isotope cycles in east antarctica
url https://acp.copernicus.org/articles/22/15637/2022/acp-22-15637-2022.pdf
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