Untersuchungen an Eisbohrkernen von Alpengletschern
Cold alpine glaciers are archives of climatic Parameters. Core drilling in alpine glaciers allows to collect ice samples of ages up to 1000 years. First results from analyses of an ice core from Colle Gnifetti (Swiss Alps) show already interesting results. Frequent occurring dust bands contain mainl...
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Copernicus Publications
1985
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Online Access: | https://dx.doi.org/10.48350/158816 https://boris.unibe.ch/158816/ |
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ftdatacite:10.48350/158816 2023-05-15T16:38:44+02:00 Untersuchungen an Eisbohrkernen von Alpengletschern Stauffer, B. Schotterer, U. 1985 https://dx.doi.org/10.48350/158816 https://boris.unibe.ch/158816/ unknown Copernicus Publications open access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 CC-BY 530 Physics Text article-journal journal article ScholarlyArticle 1985 ftdatacite https://doi.org/10.48350/158816 2021-11-05T12:55:41Z Cold alpine glaciers are archives of climatic Parameters. Core drilling in alpine glaciers allows to collect ice samples of ages up to 1000 years. First results from analyses of an ice core from Colle Gnifetti (Swiss Alps) show already interesting results. Frequent occurring dust bands contain mainly dust from the Sahara and are therefore characteristic for precipitations transported with subtropic air masses. An increase of the acidity of the precipitations starting at the beginning of our Century is most probably an anthropogenic effect. For the upper 10 m of the ice core, S04- and N03- concentrations have also been measured. Text ice core DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
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unknown |
topic |
530 Physics |
spellingShingle |
530 Physics Stauffer, B. Schotterer, U. Untersuchungen an Eisbohrkernen von Alpengletschern |
topic_facet |
530 Physics |
description |
Cold alpine glaciers are archives of climatic Parameters. Core drilling in alpine glaciers allows to collect ice samples of ages up to 1000 years. First results from analyses of an ice core from Colle Gnifetti (Swiss Alps) show already interesting results. Frequent occurring dust bands contain mainly dust from the Sahara and are therefore characteristic for precipitations transported with subtropic air masses. An increase of the acidity of the precipitations starting at the beginning of our Century is most probably an anthropogenic effect. For the upper 10 m of the ice core, S04- and N03- concentrations have also been measured. |
format |
Text |
author |
Stauffer, B. Schotterer, U. |
author_facet |
Stauffer, B. Schotterer, U. |
author_sort |
Stauffer, B. |
title |
Untersuchungen an Eisbohrkernen von Alpengletschern |
title_short |
Untersuchungen an Eisbohrkernen von Alpengletschern |
title_full |
Untersuchungen an Eisbohrkernen von Alpengletschern |
title_fullStr |
Untersuchungen an Eisbohrkernen von Alpengletschern |
title_full_unstemmed |
Untersuchungen an Eisbohrkernen von Alpengletschern |
title_sort |
untersuchungen an eisbohrkernen von alpengletschern |
publisher |
Copernicus Publications |
publishDate |
1985 |
url |
https://dx.doi.org/10.48350/158816 https://boris.unibe.ch/158816/ |
genre |
ice core |
genre_facet |
ice core |
op_rights |
open access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.48350/158816 |
_version_ |
1766029067833835520 |