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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Main Authors: Jackson, Sarah Louise, Vance, Tessa R., Crockart, Camilla, Moy, Andrew, Plummer, Christopher, Abram, Nerilie J.
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2022-1171
https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1171/
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spelling 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)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language 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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