Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya, Eurasian Arctic

A deep ice core has been drilled on Akademii Nauk ice cap, Severnaya Zemlya, Eurasian Arctic. High-resolution chemical analysis has been carried out for the upper 53 m of this ice core to study its potential as an atmospheric aerosol archive, despite strong meltwater percolation. These records show...

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Published in:Journal of Glaciology
Main Authors: Weiler, Karin, Fischer, Hubertus, Fritzsche, Diedrich, Ruth, Urs, Wilhelms, Frank, Miller, Heinz
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society 2005
Subjects:
Online Access:https://boris.unibe.ch/158292/1/weiler05jg.pdf
https://boris.unibe.ch/158292/
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spelling ftunivbern:oai:boris.unibe.ch:158292 2023-08-20T04:02:53+02:00 Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya, Eurasian Arctic Weiler, Karin Fischer, Hubertus Fritzsche, Diedrich Ruth, Urs Wilhelms, Frank Miller, Heinz 2005 application/pdf https://boris.unibe.ch/158292/1/weiler05jg.pdf https://boris.unibe.ch/158292/ eng eng International Glaciological Society https://boris.unibe.ch/158292/ info:eu-repo/semantics/restrictedAccess Weiler, Karin; Fischer, Hubertus; Fritzsche, Diedrich; Ruth, Urs; Wilhelms, Frank; Miller, Heinz (2005). Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya, Eurasian Arctic. Journal of glaciology, 51(172), pp. 64-74. International Glaciological Society 10.3189/172756505781829629 <http://dx.doi.org/10.3189/172756505781829629> 530 Physics info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed 2005 ftunivbern https://doi.org/10.3189/172756505781829629 2023-07-31T22:08:01Z A deep ice core has been drilled on Akademii Nauk ice cap, Severnaya Zemlya, Eurasian Arctic. High-resolution chemical analysis has been carried out for the upper 53 m of this ice core to study its potential as an atmospheric aerosol archive, despite strong meltwater percolation. These records show that a seasonal atmospheric signal cannot be deduced. However, strong year-to-year variations have allowed the core to be dated, and a mean annual net mass balance of 0.46 m w.e. a-1 was deduced. The chemical signature of an extraordinarily high peak in electrical conductivity at 26 m depth pointed clearly to the eruption of Bezymianny, Kamchatka, in 1956. However, in general, peaks in the electrical conductivity are not necessarily related to deposition of volcanogenic sulphur aerosol. In contrast, maximum sulphate and nitrate concentrations in the ice could be related to maximum SO2 and NOx anthropogenic emissions in the 1970s, probably caused by the nickel- and copper-producing industries in Norilsk and on the Kola peninsula or by industrial combustion processes occurring in the Siberian Arctic. In addition, during recent decades sulphate and nitrate concentrations declined by 80% and 60%, respectively, reflecting a decrease in anthropogenic pollution of the Arctic basin. Article in Journal/Newspaper Arctic Arctic Basin Arctic Ice cap ice core Journal of Glaciology Kamchatka kola peninsula norilsk Severnaya Zemlya BORIS (Bern Open Repository and Information System, University of Bern) Arctic Kola Peninsula Norilsk ENVELOPE(88.203,88.203,69.354,69.354) Severnaya Zemlya ENVELOPE(98.000,98.000,79.500,79.500) Journal of Glaciology 51 172 64 74
institution Open Polar
collection BORIS (Bern Open Repository and Information System, University of Bern)
op_collection_id ftunivbern
language English
topic 530 Physics
spellingShingle 530 Physics
Weiler, Karin
Fischer, Hubertus
Fritzsche, Diedrich
Ruth, Urs
Wilhelms, Frank
Miller, Heinz
Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya, Eurasian Arctic
topic_facet 530 Physics
description A deep ice core has been drilled on Akademii Nauk ice cap, Severnaya Zemlya, Eurasian Arctic. High-resolution chemical analysis has been carried out for the upper 53 m of this ice core to study its potential as an atmospheric aerosol archive, despite strong meltwater percolation. These records show that a seasonal atmospheric signal cannot be deduced. However, strong year-to-year variations have allowed the core to be dated, and a mean annual net mass balance of 0.46 m w.e. a-1 was deduced. The chemical signature of an extraordinarily high peak in electrical conductivity at 26 m depth pointed clearly to the eruption of Bezymianny, Kamchatka, in 1956. However, in general, peaks in the electrical conductivity are not necessarily related to deposition of volcanogenic sulphur aerosol. In contrast, maximum sulphate and nitrate concentrations in the ice could be related to maximum SO2 and NOx anthropogenic emissions in the 1970s, probably caused by the nickel- and copper-producing industries in Norilsk and on the Kola peninsula or by industrial combustion processes occurring in the Siberian Arctic. In addition, during recent decades sulphate and nitrate concentrations declined by 80% and 60%, respectively, reflecting a decrease in anthropogenic pollution of the Arctic basin.
format Article in Journal/Newspaper
author Weiler, Karin
Fischer, Hubertus
Fritzsche, Diedrich
Ruth, Urs
Wilhelms, Frank
Miller, Heinz
author_facet Weiler, Karin
Fischer, Hubertus
Fritzsche, Diedrich
Ruth, Urs
Wilhelms, Frank
Miller, Heinz
author_sort Weiler, Karin
title Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya, Eurasian Arctic
title_short Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya, Eurasian Arctic
title_full Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya, Eurasian Arctic
title_fullStr Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya, Eurasian Arctic
title_full_unstemmed Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya, Eurasian Arctic
title_sort glaciochemical reconnaissance of a new ice core from severnaya zemlya, eurasian arctic
publisher International Glaciological Society
publishDate 2005
url https://boris.unibe.ch/158292/1/weiler05jg.pdf
https://boris.unibe.ch/158292/
long_lat ENVELOPE(88.203,88.203,69.354,69.354)
ENVELOPE(98.000,98.000,79.500,79.500)
geographic Arctic
Kola Peninsula
Norilsk
Severnaya Zemlya
geographic_facet Arctic
Kola Peninsula
Norilsk
Severnaya Zemlya
genre Arctic
Arctic Basin
Arctic
Ice cap
ice core
Journal of Glaciology
Kamchatka
kola peninsula
norilsk
Severnaya Zemlya
genre_facet Arctic
Arctic Basin
Arctic
Ice cap
ice core
Journal of Glaciology
Kamchatka
kola peninsula
norilsk
Severnaya Zemlya
op_source Weiler, Karin; Fischer, Hubertus; Fritzsche, Diedrich; Ruth, Urs; Wilhelms, Frank; Miller, Heinz (2005). Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya, Eurasian Arctic. Journal of glaciology, 51(172), pp. 64-74. International Glaciological Society 10.3189/172756505781829629 <http://dx.doi.org/10.3189/172756505781829629>
op_relation https://boris.unibe.ch/158292/
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.3189/172756505781829629
container_title Journal of Glaciology
container_volume 51
container_issue 172
container_start_page 64
op_container_end_page 74
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