Changes in black carbon deposition to Antarctica from two high-resolution ice core records, 1850–2000 AD

Refractory black carbon aerosols (rBC) emitted by biomass burning (fires) and fossil fuel combustion, affect global climate and atmospheric chemistry. In the Southern Hemisphere (SH), rBC is transported in the atmosphere from low- and mid-latitudes to Antarctica and deposited to the polar ice sheet...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Bisiaux, M. M., Edwards, R., McConnell, J. R., Curran, M. A. J., Ommen, T. D., Smith, A. M., Neumann, T. A., Pasteris, D. R., Penner, J. E., Taylor, K.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/acp-12-4107-2012
https://www.atmos-chem-phys.net/12/4107/2012/
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spelling ftcopernicus:oai:publications.copernicus.org:acp12632 2023-05-15T13:45:55+02:00 Changes in black carbon deposition to Antarctica from two high-resolution ice core records, 1850–2000 AD Bisiaux, M. M. Edwards, R. McConnell, J. R. Curran, M. A. J. Ommen, T. D. Smith, A. M. Neumann, T. A. Pasteris, D. R. Penner, J. E. Taylor, K. 2018-01-15 application/pdf https://doi.org/10.5194/acp-12-4107-2012 https://www.atmos-chem-phys.net/12/4107/2012/ eng eng doi:10.5194/acp-12-4107-2012 https://www.atmos-chem-phys.net/12/4107/2012/ eISSN: 1680-7324 Text 2018 ftcopernicus https://doi.org/10.5194/acp-12-4107-2012 2019-12-24T09:56:17Z Refractory black carbon aerosols (rBC) emitted by biomass burning (fires) and fossil fuel combustion, affect global climate and atmospheric chemistry. In the Southern Hemisphere (SH), rBC is transported in the atmosphere from low- and mid-latitudes to Antarctica and deposited to the polar ice sheet preserving a history of emissions and atmospheric transport. Here, we present two high-resolution Antarctic rBC ice core records drilled from the West Antarctic Ice Sheet divide and Law Dome on the periphery of the East Antarctic ice sheet. Separated by ~3500 km, the records span calendar years 1850–2001 and reflect the rBC distribution over the Indian and Pacific ocean sectors of the Southern Ocean. Concentrations of rBC in the ice cores displayed significant variability at annual to decadal time scales, notably in ENSO-QBO and AAO frequency bands. The delay observed between rBC and ENSO variability suggested that ENSO does not directly affect rBC transport, but rather continental hydrology, subsequent fire regimes, and aerosol emissions. From 1850 to 1950, the two ice core records were uncorrelated but were highly correlated from 1950 to 2002 (cross-correlation coefficient at annual resolution: r = 0.54, p < 0.01) due to a common decrease in rBC variability. The decrease in ice-core rBC from the 1950s to late 1980s displays similarities with inventories of SH rBC grass fires and biofuel emissions, which show reduced emission estimates over that period. Text Antarc* Antarctic Antarctica ice core Ice Sheet Southern Ocean Copernicus Publications: E-Journals Antarctic East Antarctic Ice Sheet Indian Law Dome ENVELOPE(112.833,112.833,-66.733,-66.733) Pacific Southern Ocean West Antarctic Ice Sheet Atmospheric Chemistry and Physics 12 9 4107 4115
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Refractory black carbon aerosols (rBC) emitted by biomass burning (fires) and fossil fuel combustion, affect global climate and atmospheric chemistry. In the Southern Hemisphere (SH), rBC is transported in the atmosphere from low- and mid-latitudes to Antarctica and deposited to the polar ice sheet preserving a history of emissions and atmospheric transport. Here, we present two high-resolution Antarctic rBC ice core records drilled from the West Antarctic Ice Sheet divide and Law Dome on the periphery of the East Antarctic ice sheet. Separated by ~3500 km, the records span calendar years 1850–2001 and reflect the rBC distribution over the Indian and Pacific ocean sectors of the Southern Ocean. Concentrations of rBC in the ice cores displayed significant variability at annual to decadal time scales, notably in ENSO-QBO and AAO frequency bands. The delay observed between rBC and ENSO variability suggested that ENSO does not directly affect rBC transport, but rather continental hydrology, subsequent fire regimes, and aerosol emissions. From 1850 to 1950, the two ice core records were uncorrelated but were highly correlated from 1950 to 2002 (cross-correlation coefficient at annual resolution: r = 0.54, p < 0.01) due to a common decrease in rBC variability. The decrease in ice-core rBC from the 1950s to late 1980s displays similarities with inventories of SH rBC grass fires and biofuel emissions, which show reduced emission estimates over that period.
format Text
author Bisiaux, M. M.
Edwards, R.
McConnell, J. R.
Curran, M. A. J.
Ommen, T. D.
Smith, A. M.
Neumann, T. A.
Pasteris, D. R.
Penner, J. E.
Taylor, K.
spellingShingle Bisiaux, M. M.
Edwards, R.
McConnell, J. R.
Curran, M. A. J.
Ommen, T. D.
Smith, A. M.
Neumann, T. A.
Pasteris, D. R.
Penner, J. E.
Taylor, K.
Changes in black carbon deposition to Antarctica from two high-resolution ice core records, 1850–2000 AD
author_facet Bisiaux, M. M.
Edwards, R.
McConnell, J. R.
Curran, M. A. J.
Ommen, T. D.
Smith, A. M.
Neumann, T. A.
Pasteris, D. R.
Penner, J. E.
Taylor, K.
author_sort Bisiaux, M. M.
title Changes in black carbon deposition to Antarctica from two high-resolution ice core records, 1850–2000 AD
title_short Changes in black carbon deposition to Antarctica from two high-resolution ice core records, 1850–2000 AD
title_full Changes in black carbon deposition to Antarctica from two high-resolution ice core records, 1850–2000 AD
title_fullStr Changes in black carbon deposition to Antarctica from two high-resolution ice core records, 1850–2000 AD
title_full_unstemmed Changes in black carbon deposition to Antarctica from two high-resolution ice core records, 1850–2000 AD
title_sort changes in black carbon deposition to antarctica from two high-resolution ice core records, 1850–2000 ad
publishDate 2018
url https://doi.org/10.5194/acp-12-4107-2012
https://www.atmos-chem-phys.net/12/4107/2012/
long_lat ENVELOPE(112.833,112.833,-66.733,-66.733)
geographic Antarctic
East Antarctic Ice Sheet
Indian
Law Dome
Pacific
Southern Ocean
West Antarctic Ice Sheet
geographic_facet Antarctic
East Antarctic Ice Sheet
Indian
Law Dome
Pacific
Southern Ocean
West Antarctic Ice Sheet
genre Antarc*
Antarctic
Antarctica
ice core
Ice Sheet
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctica
ice core
Ice Sheet
Southern Ocean
op_source eISSN: 1680-7324
op_relation doi:10.5194/acp-12-4107-2012
https://www.atmos-chem-phys.net/12/4107/2012/
op_doi https://doi.org/10.5194/acp-12-4107-2012
container_title Atmospheric Chemistry and Physics
container_volume 12
container_issue 9
container_start_page 4107
op_container_end_page 4115
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