Nine Centuries of Microparticle Deposition at the South Pole

Abstract The analysis of microparticles in a 101-m core from Amundsen-Scott South Pole Station, Antarctica has revealed a substantial increase in total particle concentration between approximately 1450 and 1850 A.D., a period encompassing the latest neoglacial interval or Little Ice Age. It is likel...

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Published in:Quaternary Research
Main Authors: Mosley-Thompson, E., Thompson, L. G.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1982
Subjects:
Online Access:http://dx.doi.org/10.1016/0033-5894(82)90041-2
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spelling crcambridgeupr:10.1016/0033-5894(82)90041-2 2024-06-09T07:38:20+00:00 Nine Centuries of Microparticle Deposition at the South Pole Mosley-Thompson, E. Thompson, L. G. 1982 http://dx.doi.org/10.1016/0033-5894(82)90041-2 http://api.elsevier.com/content/article/PII:0033589482900412?httpAccept=text/xml http://api.elsevier.com/content/article/PII:0033589482900412?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400021979 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 17, issue 1, page 1-13 ISSN 0033-5894 1096-0287 journal-article 1982 crcambridgeupr https://doi.org/10.1016/0033-5894(82)90041-2 2024-05-15T13:13:26Z Abstract The analysis of microparticles in a 101-m core from Amundsen-Scott South Pole Station, Antarctica has revealed a substantial increase in total particle concentration between approximately 1450 and 1850 A.D., a period encompassing the latest neoglacial interval or Little Ice Age. It is likely that this reflects a simultaneous increase in the concentration of particulate material in the Antarctic atmosphere. This is important climatologically, for the Antarctic atmosphere may represent the closest approximation to the natural background aerosol. Thus cores from East Antarctica may contain long and detailed records of the natural global background aerosol. Such records are unavailable from any other medium. Additionally, a cyclical variation which appears to be annual has been detected in the South Pole particle record. These features allow construction of a relative time scale for ice cores older than 100 yr from regions of low accumulation (<10 g a −1 ) where many traditional techniques are not applicable. This is especially significant, as the comparison of climatic data extracted from ice cores with other records of proxy data depends upon the ability to assign an accurate time scale to the ice core. An estimated nine-century record of net annual accumulation at the South Pole has been compiled and the calculated error in the time scale is ±90 yr. Article in Journal/Newspaper Amundsen-Scott Antarc* Antarctic Antarctica East Antarctica ice core South pole South pole Cambridge University Press Amundsen Scott South Pole Station ENVELOPE(0.000,0.000,-90.000,-90.000) Amundsen-Scott ENVELOPE(0.000,0.000,-90.000,-90.000) Amundsen-Scott South Pole Station ENVELOPE(139.273,139.273,-89.998,-89.998) Antarctic East Antarctica South Pole The Antarctic Quaternary Research 17 1 1 13
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description Abstract The analysis of microparticles in a 101-m core from Amundsen-Scott South Pole Station, Antarctica has revealed a substantial increase in total particle concentration between approximately 1450 and 1850 A.D., a period encompassing the latest neoglacial interval or Little Ice Age. It is likely that this reflects a simultaneous increase in the concentration of particulate material in the Antarctic atmosphere. This is important climatologically, for the Antarctic atmosphere may represent the closest approximation to the natural background aerosol. Thus cores from East Antarctica may contain long and detailed records of the natural global background aerosol. Such records are unavailable from any other medium. Additionally, a cyclical variation which appears to be annual has been detected in the South Pole particle record. These features allow construction of a relative time scale for ice cores older than 100 yr from regions of low accumulation (<10 g a −1 ) where many traditional techniques are not applicable. This is especially significant, as the comparison of climatic data extracted from ice cores with other records of proxy data depends upon the ability to assign an accurate time scale to the ice core. An estimated nine-century record of net annual accumulation at the South Pole has been compiled and the calculated error in the time scale is ±90 yr.
format Article in Journal/Newspaper
author Mosley-Thompson, E.
Thompson, L. G.
spellingShingle Mosley-Thompson, E.
Thompson, L. G.
Nine Centuries of Microparticle Deposition at the South Pole
author_facet Mosley-Thompson, E.
Thompson, L. G.
author_sort Mosley-Thompson, E.
title Nine Centuries of Microparticle Deposition at the South Pole
title_short Nine Centuries of Microparticle Deposition at the South Pole
title_full Nine Centuries of Microparticle Deposition at the South Pole
title_fullStr Nine Centuries of Microparticle Deposition at the South Pole
title_full_unstemmed Nine Centuries of Microparticle Deposition at the South Pole
title_sort nine centuries of microparticle deposition at the south pole
publisher Cambridge University Press (CUP)
publishDate 1982
url http://dx.doi.org/10.1016/0033-5894(82)90041-2
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long_lat ENVELOPE(0.000,0.000,-90.000,-90.000)
ENVELOPE(0.000,0.000,-90.000,-90.000)
ENVELOPE(139.273,139.273,-89.998,-89.998)
geographic Amundsen Scott South Pole Station
Amundsen-Scott
Amundsen-Scott South Pole Station
Antarctic
East Antarctica
South Pole
The Antarctic
geographic_facet Amundsen Scott South Pole Station
Amundsen-Scott
Amundsen-Scott South Pole Station
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East Antarctica
South Pole
The Antarctic
genre Amundsen-Scott
Antarc*
Antarctic
Antarctica
East Antarctica
ice core
South pole
South pole
genre_facet Amundsen-Scott
Antarc*
Antarctic
Antarctica
East Antarctica
ice core
South pole
South pole
op_source Quaternary Research
volume 17, issue 1, page 1-13
ISSN 0033-5894 1096-0287
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