Climatology of the Mount Brown South ice core site in East Antarctica: implications for the interpretation of a water isotope record
Water stable isotope records from ice cores ( δ 18 O and δ D) are a critical tool for constraining long-term temperature variability at high latitudes. However, precipitation in Antarctica consists of semi-continuous small events and intermittent extreme events. In regions of high accumulation, this...
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ftcopernicus:oai:publications.copernicus.org:egusphere107444 2023-09-05T13:15:26+02:00 Climatology of the Mount Brown South ice core site in East Antarctica: implications for the interpretation of a water isotope record Jackson, Sarah Louise Vance, Tessa R. Crockart, Camilla Moy, Andrew Plummer, Christopher Abram, Nerilie J. 2023-08-14 application/pdf https://doi.org/10.5194/egusphere-2022-1171 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1171/ eng eng doi:10.5194/egusphere-2022-1171 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1171/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2022-1171 2023-08-21T16:24:16Z Water stable isotope records from ice cores ( δ 18 O and δ D) are a critical tool for constraining long-term temperature variability at high latitudes. However, precipitation in Antarctica consists of semi-continuous small events and intermittent extreme events. In regions of high accumulation, this can bias ice core records towards recording the synoptic climate conditions present during extreme precipitation events. In this study we utilise a combination of ice core data, reanalysis products, and models to understand how precipitation intermittency impacts the temperature records preserved in an ice core from Mount Brown South in East Antarctica. Extreme precipitation events represent only the largest 10 % of all precipitation events, but they account for 52 % of the total annual snowfall at this site, leading to an overrepresentation of these events in the ice core record. Extreme precipitation events are associated with high-pressure systems in the mid-latitudes that cause increased transport of warm and moist air from the southern Indian Ocean to the ice core site. Warm temperatures associated with these events result in a +4.8 ∘ C warm bias in the mean annual temperature when weighted by daily precipitation, and water isotopes in the Mount Brown South ice core are shown to be significantly correlated with local temperature when this precipitation-induced temperature bias is included. The Mount Brown South water isotope record spans more than 1000 years and will provide a valuable regional reconstruction of long-term temperature and hydroclimate variability in the data-sparse southern Indian Ocean region. Text Antarc* Antarctica East Antarctica ice core Copernicus Publications: E-Journals East Antarctica Indian Mount Brown ENVELOPE(86.000,86.000,-68.617,-68.617) South Ice ENVELOPE(-29.867,-29.867,-81.950,-81.950) |
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Copernicus Publications: E-Journals |
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English |
description |
Water stable isotope records from ice cores ( δ 18 O and δ D) are a critical tool for constraining long-term temperature variability at high latitudes. However, precipitation in Antarctica consists of semi-continuous small events and intermittent extreme events. In regions of high accumulation, this can bias ice core records towards recording the synoptic climate conditions present during extreme precipitation events. In this study we utilise a combination of ice core data, reanalysis products, and models to understand how precipitation intermittency impacts the temperature records preserved in an ice core from Mount Brown South in East Antarctica. Extreme precipitation events represent only the largest 10 % of all precipitation events, but they account for 52 % of the total annual snowfall at this site, leading to an overrepresentation of these events in the ice core record. Extreme precipitation events are associated with high-pressure systems in the mid-latitudes that cause increased transport of warm and moist air from the southern Indian Ocean to the ice core site. Warm temperatures associated with these events result in a +4.8 ∘ C warm bias in the mean annual temperature when weighted by daily precipitation, and water isotopes in the Mount Brown South ice core are shown to be significantly correlated with local temperature when this precipitation-induced temperature bias is included. The Mount Brown South water isotope record spans more than 1000 years and will provide a valuable regional reconstruction of long-term temperature and hydroclimate variability in the data-sparse southern Indian Ocean region. |
format |
Text |
author |
Jackson, Sarah Louise Vance, Tessa R. Crockart, Camilla Moy, Andrew Plummer, Christopher Abram, Nerilie J. |
spellingShingle |
Jackson, Sarah Louise Vance, Tessa R. Crockart, Camilla Moy, Andrew Plummer, Christopher Abram, Nerilie J. Climatology of the Mount Brown South ice core site in East Antarctica: implications for the interpretation of a water isotope record |
author_facet |
Jackson, Sarah Louise Vance, Tessa R. Crockart, Camilla Moy, Andrew Plummer, Christopher Abram, Nerilie J. |
author_sort |
Jackson, Sarah Louise |
title |
Climatology of the Mount Brown South ice core site in East Antarctica: implications for the interpretation of a water isotope record |
title_short |
Climatology of the Mount Brown South ice core site in East Antarctica: implications for the interpretation of a water isotope record |
title_full |
Climatology of the Mount Brown South ice core site in East Antarctica: implications for the interpretation of a water isotope record |
title_fullStr |
Climatology of the Mount Brown South ice core site in East Antarctica: implications for the interpretation of a water isotope record |
title_full_unstemmed |
Climatology of the Mount Brown South ice core site in East Antarctica: implications for the interpretation of a water isotope record |
title_sort |
climatology of the mount brown south ice core site in east antarctica: implications for the interpretation of a water isotope record |
publishDate |
2023 |
url |
https://doi.org/10.5194/egusphere-2022-1171 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1171/ |
long_lat |
ENVELOPE(86.000,86.000,-68.617,-68.617) ENVELOPE(-29.867,-29.867,-81.950,-81.950) |
geographic |
East Antarctica Indian Mount Brown South Ice |
geographic_facet |
East Antarctica Indian Mount Brown South Ice |
genre |
Antarc* Antarctica East Antarctica ice core |
genre_facet |
Antarc* Antarctica East Antarctica ice core |
op_source |
eISSN: |
op_relation |
doi:10.5194/egusphere-2022-1171 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1171/ |
op_doi |
https://doi.org/10.5194/egusphere-2022-1171 |
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1776197254538854400 |