Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya

A deep ice core has been drilled on the Akademii Nauk ice cap, Severnaya Zemlya. High resolution chemical analyses has been carried out for the upper 53m of this ice core to study its potential as an atmospheric aerosol archive despite strong melt water percolation. These records show that a seasona...

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Published in:Journal of Glaciology
Main Authors: Weiler, K., Fischer, Hubertus, Fritzsche, Diedrich, Ruth, Urs, Wilhelms, Frank, Miller, Heinrich
Format: Article in Journal/Newspaper
Language:unknown
Published: 2005
Subjects:
Online Access:https://epic.awi.de/id/eprint/9893/
https://epic.awi.de/id/eprint/9893/1/Wei2003d.pdf
https://hdl.handle.net/10013/epic.20389
https://hdl.handle.net/10013/epic.20389.d001
id ftawi:oai:epic.awi.de:9893
record_format openpolar
spelling ftawi:oai:epic.awi.de:9893 2023-09-05T13:16:01+02:00 Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya Weiler, K. Fischer, Hubertus Fritzsche, Diedrich Ruth, Urs Wilhelms, Frank Miller, Heinrich 2005 application/pdf https://epic.awi.de/id/eprint/9893/ https://epic.awi.de/id/eprint/9893/1/Wei2003d.pdf https://hdl.handle.net/10013/epic.20389 https://hdl.handle.net/10013/epic.20389.d001 unknown https://epic.awi.de/id/eprint/9893/1/Wei2003d.pdf https://hdl.handle.net/10013/epic.20389.d001 Weiler, K. , Fischer, H. , Fritzsche, D. orcid:0000-0002-0018-8993 , Ruth, U. , Wilhelms, F. orcid:0000-0001-7688-3135 and Miller, H. (2005) Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya , Journal of Glaciology, 51 (172), pp. 64-74 . doi:10.3189/172756505781829629 <https://doi.org/10.3189/172756505781829629> , hdl:10013/epic.20389 EPIC3Journal of Glaciology, 51(172), pp. 64-74, ISSN: 0022-1430 Article isiRev 2005 ftawi https://doi.org/10.3189/172756505781829629 2023-08-22T19:48:19Z A deep ice core has been drilled on the Akademii Nauk ice cap, Severnaya Zemlya. High resolution chemical analyses has been carried out for the upper 53m of this ice core to study its potential as an atmospheric aerosol archive despite strong melt water 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 water equivalent per yearcould be deduced. The chemical signature of an extraordinary high peak in electrical conductivity at 26m depth pointed clearly to the eruption of Bezymianny, Kamtchatka, in 1956. However, in general, peaks in the electrical conductivity are not necessarily related to deposition of volcanogenic sulfur aerosol. In contrast, maximum sulfate 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 sulfate and nitrate concentrations declined by 80% and 60% respectively reflecting a decrease in anthropogenic pollution of the Arctic basin. Article in Journal/Newspaper Arctic Basin Arctic Ice cap ice core Journal of Glaciology kola peninsula norilsk Severnaya Zemlya Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) 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 Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description A deep ice core has been drilled on the Akademii Nauk ice cap, Severnaya Zemlya. High resolution chemical analyses has been carried out for the upper 53m of this ice core to study its potential as an atmospheric aerosol archive despite strong melt water 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 water equivalent per yearcould be deduced. The chemical signature of an extraordinary high peak in electrical conductivity at 26m depth pointed clearly to the eruption of Bezymianny, Kamtchatka, in 1956. However, in general, peaks in the electrical conductivity are not necessarily related to deposition of volcanogenic sulfur aerosol. In contrast, maximum sulfate 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 sulfate 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, K.
Fischer, Hubertus
Fritzsche, Diedrich
Ruth, Urs
Wilhelms, Frank
Miller, Heinrich
spellingShingle Weiler, K.
Fischer, Hubertus
Fritzsche, Diedrich
Ruth, Urs
Wilhelms, Frank
Miller, Heinrich
Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya
author_facet Weiler, K.
Fischer, Hubertus
Fritzsche, Diedrich
Ruth, Urs
Wilhelms, Frank
Miller, Heinrich
author_sort Weiler, K.
title Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya
title_short Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya
title_full Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya
title_fullStr Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya
title_full_unstemmed Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya
title_sort glaciochemical reconnaissance of a new ice core from severnaya zemlya
publishDate 2005
url https://epic.awi.de/id/eprint/9893/
https://epic.awi.de/id/eprint/9893/1/Wei2003d.pdf
https://hdl.handle.net/10013/epic.20389
https://hdl.handle.net/10013/epic.20389.d001
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 Basin
Arctic
Ice cap
ice core
Journal of Glaciology
kola peninsula
norilsk
Severnaya Zemlya
genre_facet Arctic Basin
Arctic
Ice cap
ice core
Journal of Glaciology
kola peninsula
norilsk
Severnaya Zemlya
op_source EPIC3Journal of Glaciology, 51(172), pp. 64-74, ISSN: 0022-1430
op_relation https://epic.awi.de/id/eprint/9893/1/Wei2003d.pdf
https://hdl.handle.net/10013/epic.20389.d001
Weiler, K. , Fischer, H. , Fritzsche, D. orcid:0000-0002-0018-8993 , Ruth, U. , Wilhelms, F. orcid:0000-0001-7688-3135 and Miller, H. (2005) Glaciochemical reconnaissance of a new ice core from Severnaya Zemlya , Journal of Glaciology, 51 (172), pp. 64-74 . doi:10.3189/172756505781829629 <https://doi.org/10.3189/172756505781829629> , hdl:10013/epic.20389
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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