Glaciochemical dating of an ice core from upper Grenzgletscher (4200 m a.s.l.)
One crucial condition for the interpretation of ice-core records is the establishment of an accurate time-scale. This task is especially difficult for glacier sites in a complex topography such as the Alps, due to the often irregular deposition of fresh precipitation. In this work, dating techniques...
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International Glaciological Society
2000
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Online Access: | https://doi.org/10.3189/172756500781833098 |
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fteawag:oai:dora:eawag_4097 2023-05-15T16:38:38+02:00 Glaciochemical dating of an ice core from upper Grenzgletscher (4200 m a.s.l.) Eichler, Anja Schwikowski, Margit Gäggeler, Heinz W. Furrer, Verena Synal, Hans-Arno Beer, Jürg Saurer, Matthias Funk, Martin 2000 https://doi.org/10.3189/172756500781833098 eng eng International Glaciological Society Journal of Glaciology--J. Glaciol.--journals:1633--0022-1430 eawag:4097 journal id: journals:1633 issn: 0022-1430 ut: 000165920700017 local: 5626 doi:10.3189/172756500781833098 scopus: 2-s2.0-0034514759 Text Journal Article 2000 fteawag https://doi.org/10.3189/172756500781833098 2023-04-09T04:48:23Z One crucial condition for the interpretation of ice-core records is the establishment of an accurate time-scale. This task is especially difficult for glacier sites in a complex topography such as the Alps, due to the often irregular deposition of fresh precipitation. In this work, dating techniques were applied to an Alpine ice core from upper Grenzgletscher; Monte Rosa massif (4200 m a.s.l.), representing about two-thirds of the total glacier thickness. They are leased on (i) the radioactive decay of the isotope 210 Pb, (ii) seasonally varying signals such as the concentrations of NH 4 + and the isotopic ratio δ 18 O, and (iii) stratigraphic markers from Saharan dust falls, atmospheric nuclear weapon tests and the reactor accident in Chernobyl. From the combined application of these dating methods, a time period of 1937–94 covered by the ice core was derived. Dating uncertainty is <1 year for the period 1970–94 and ±2 years for the period 1937–69. The observed thinning of the annual layers as a function of depth could be well described by a simple kinematic glacier flow model. Article in Journal/Newspaper ice core Journal of Glaciology DORA Eawag Monte Rosa ENVELOPE(162.850,162.850,-70.917,-70.917) Journal of Glaciology 46 154 507 515 |
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fteawag |
language |
English |
description |
One crucial condition for the interpretation of ice-core records is the establishment of an accurate time-scale. This task is especially difficult for glacier sites in a complex topography such as the Alps, due to the often irregular deposition of fresh precipitation. In this work, dating techniques were applied to an Alpine ice core from upper Grenzgletscher; Monte Rosa massif (4200 m a.s.l.), representing about two-thirds of the total glacier thickness. They are leased on (i) the radioactive decay of the isotope 210 Pb, (ii) seasonally varying signals such as the concentrations of NH 4 + and the isotopic ratio δ 18 O, and (iii) stratigraphic markers from Saharan dust falls, atmospheric nuclear weapon tests and the reactor accident in Chernobyl. From the combined application of these dating methods, a time period of 1937–94 covered by the ice core was derived. Dating uncertainty is <1 year for the period 1970–94 and ±2 years for the period 1937–69. The observed thinning of the annual layers as a function of depth could be well described by a simple kinematic glacier flow model. |
format |
Article in Journal/Newspaper |
author |
Eichler, Anja Schwikowski, Margit Gäggeler, Heinz W. Furrer, Verena Synal, Hans-Arno Beer, Jürg Saurer, Matthias Funk, Martin |
spellingShingle |
Eichler, Anja Schwikowski, Margit Gäggeler, Heinz W. Furrer, Verena Synal, Hans-Arno Beer, Jürg Saurer, Matthias Funk, Martin Glaciochemical dating of an ice core from upper Grenzgletscher (4200 m a.s.l.) |
author_facet |
Eichler, Anja Schwikowski, Margit Gäggeler, Heinz W. Furrer, Verena Synal, Hans-Arno Beer, Jürg Saurer, Matthias Funk, Martin |
author_sort |
Eichler, Anja |
title |
Glaciochemical dating of an ice core from upper Grenzgletscher (4200 m a.s.l.) |
title_short |
Glaciochemical dating of an ice core from upper Grenzgletscher (4200 m a.s.l.) |
title_full |
Glaciochemical dating of an ice core from upper Grenzgletscher (4200 m a.s.l.) |
title_fullStr |
Glaciochemical dating of an ice core from upper Grenzgletscher (4200 m a.s.l.) |
title_full_unstemmed |
Glaciochemical dating of an ice core from upper Grenzgletscher (4200 m a.s.l.) |
title_sort |
glaciochemical dating of an ice core from upper grenzgletscher (4200 m a.s.l.) |
publisher |
International Glaciological Society |
publishDate |
2000 |
url |
https://doi.org/10.3189/172756500781833098 |
long_lat |
ENVELOPE(162.850,162.850,-70.917,-70.917) |
geographic |
Monte Rosa |
geographic_facet |
Monte Rosa |
genre |
ice core Journal of Glaciology |
genre_facet |
ice core Journal of Glaciology |
op_relation |
Journal of Glaciology--J. Glaciol.--journals:1633--0022-1430 eawag:4097 journal id: journals:1633 issn: 0022-1430 ut: 000165920700017 local: 5626 doi:10.3189/172756500781833098 scopus: 2-s2.0-0034514759 |
op_doi |
https://doi.org/10.3189/172756500781833098 |
container_title |
Journal of Glaciology |
container_volume |
46 |
container_issue |
154 |
container_start_page |
507 |
op_container_end_page |
515 |
_version_ |
1766028944940728320 |