Dust and calcium record in calculated for ice core EPICA Dome C ...

Ice core data from Antarctica provide detailed insights into the characteristics of past climate, atmospheric circulation, as well as changes in the aerosol load of the atmosphere. We present high-resolution records of soluble calcium (Ca2+), non-sea-salt soluble calcium (nssCa2+), and particulate m...

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Main Authors: Lambert, Fabrice, Bigler, Matthias, Steffensen, Jørgen Peder, Hutterli, Manuel A, Fischer, Hubertus
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2012
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.779311
https://doi.pangaea.de/10.1594/PANGAEA.779311
id ftdatacite:10.1594/pangaea.779311
record_format openpolar
spelling ftdatacite:10.1594/pangaea.779311 2024-09-15T17:47:16+00:00 Dust and calcium record in calculated for ice core EPICA Dome C ... Lambert, Fabrice Bigler, Matthias Steffensen, Jørgen Peder Hutterli, Manuel A Fischer, Hubertus 2012 application/zip https://dx.doi.org/10.1594/pangaea.779311 https://doi.pangaea.de/10.1594/PANGAEA.779311 en eng PANGAEA https://dx.doi.org/10.5194/cp-8-609-2012 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Ice drill Dome C European Project for Ice Coring in Antarctica EPICA article Collection Supplementary Publication Series of Datasets 2012 ftdatacite https://doi.org/10.1594/pangaea.77931110.5194/cp-8-609-2012 2024-08-01T10:59:28Z Ice core data from Antarctica provide detailed insights into the characteristics of past climate, atmospheric circulation, as well as changes in the aerosol load of the atmosphere. We present high-resolution records of soluble calcium (Ca2+), non-sea-salt soluble calcium (nssCa2+), and particulate mineral dust aerosol from the East Antarctic Plateau at a depth resolution of 1 cm, spanning the past 800 000 years. Despite the fact that all three parameters are largely dust-derived, the ratio of nssCa2+ to particulate dust is dependent on the particulate dust concentration itself. We used principal component analysis to extract the joint climatic signal and produce a common high-resolution record of dust flux. This new record is used to identify Antarctic warming events during the past eight glacial periods. The phasing of dust flux and CO2 changes during glacial-interglacial transitions reveals that iron fertilization of the Southern Ocean during the past nine glacial terminations was not the dominant factor ... : Supplement to: Lambert, Fabrice; Bigler, Matthias; Steffensen, Jørgen Peder; Hutterli, Manuel A; Fischer, Hubertus (2012): Centennial mineral dust variability in high-resolution ice core data from Dome C, Antarctica. Climate of the Past, 8, 609-623 ... Article in Journal/Newspaper Antarc* Antarctic Antarctica EPICA ice core Southern Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Ice drill
Dome C
European Project for Ice Coring in Antarctica EPICA
spellingShingle Ice drill
Dome C
European Project for Ice Coring in Antarctica EPICA
Lambert, Fabrice
Bigler, Matthias
Steffensen, Jørgen Peder
Hutterli, Manuel A
Fischer, Hubertus
Dust and calcium record in calculated for ice core EPICA Dome C ...
topic_facet Ice drill
Dome C
European Project for Ice Coring in Antarctica EPICA
description Ice core data from Antarctica provide detailed insights into the characteristics of past climate, atmospheric circulation, as well as changes in the aerosol load of the atmosphere. We present high-resolution records of soluble calcium (Ca2+), non-sea-salt soluble calcium (nssCa2+), and particulate mineral dust aerosol from the East Antarctic Plateau at a depth resolution of 1 cm, spanning the past 800 000 years. Despite the fact that all three parameters are largely dust-derived, the ratio of nssCa2+ to particulate dust is dependent on the particulate dust concentration itself. We used principal component analysis to extract the joint climatic signal and produce a common high-resolution record of dust flux. This new record is used to identify Antarctic warming events during the past eight glacial periods. The phasing of dust flux and CO2 changes during glacial-interglacial transitions reveals that iron fertilization of the Southern Ocean during the past nine glacial terminations was not the dominant factor ... : Supplement to: Lambert, Fabrice; Bigler, Matthias; Steffensen, Jørgen Peder; Hutterli, Manuel A; Fischer, Hubertus (2012): Centennial mineral dust variability in high-resolution ice core data from Dome C, Antarctica. Climate of the Past, 8, 609-623 ...
format Article in Journal/Newspaper
author Lambert, Fabrice
Bigler, Matthias
Steffensen, Jørgen Peder
Hutterli, Manuel A
Fischer, Hubertus
author_facet Lambert, Fabrice
Bigler, Matthias
Steffensen, Jørgen Peder
Hutterli, Manuel A
Fischer, Hubertus
author_sort Lambert, Fabrice
title Dust and calcium record in calculated for ice core EPICA Dome C ...
title_short Dust and calcium record in calculated for ice core EPICA Dome C ...
title_full Dust and calcium record in calculated for ice core EPICA Dome C ...
title_fullStr Dust and calcium record in calculated for ice core EPICA Dome C ...
title_full_unstemmed Dust and calcium record in calculated for ice core EPICA Dome C ...
title_sort dust and calcium record in calculated for ice core epica dome c ...
publisher PANGAEA
publishDate 2012
url https://dx.doi.org/10.1594/pangaea.779311
https://doi.pangaea.de/10.1594/PANGAEA.779311
genre Antarc*
Antarctic
Antarctica
EPICA
ice core
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctica
EPICA
ice core
Southern Ocean
op_relation https://dx.doi.org/10.5194/cp-8-609-2012
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.77931110.5194/cp-8-609-2012
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