Zum Problem der Stabilität der Klimabedingungen in Westsibirien während der Glaziale und Interglaziale
The depression values of the summer temperature and also of the mean annual temperature in Western Siberia during the last glaciation, have been deduced. This calculation has been based on the different position of the boreal boundaries of the tundra and the continental deciduous forests during the...
Published in: | E&G Quaternary Science Journal |
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Language: | English |
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Geozon Science Media
1960
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00039725 2023-05-15T15:07:50+02:00 Zum Problem der Stabilität der Klimabedingungen in Westsibirien während der Glaziale und Interglaziale Weischet, W. 1960-12 electronic https://doi.org/10.3285/eg.11.1.09 https://noa.gwlb.de/receive/cop_mods_00039725 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00039402/egqsj-11-77-1960.pdf https://egqsj.copernicus.org/articles/11/77/1960/egqsj-11-77-1960.pdf eng eng Geozon Science Media E&G Quaternary Science Journal -- Quaternary science journal -- http://www.bibliothek.uni-regensburg.de/ezeit/?2572732 -- https://www.eg-quaternary-sci-j.net/volumes.html -- 2199-9090 https://doi.org/10.3285/eg.11.1.09 https://noa.gwlb.de/receive/cop_mods_00039725 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00039402/egqsj-11-77-1960.pdf https://egqsj.copernicus.org/articles/11/77/1960/egqsj-11-77-1960.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 1960 ftnonlinearchiv https://doi.org/10.3285/eg.11.1.09 2022-02-08T22:42:26Z The depression values of the summer temperature and also of the mean annual temperature in Western Siberia during the last glaciation, have been deduced. This calculation has been based on the different position of the boreal boundaries of the tundra and the continental deciduous forests during the ice ages and at the present time. According to these calculations the following depressions of summer temperature have been obtained: 5-8° C near the arctic circle and 2-4° C in the latitude of 50° North, in comparison with the 10-12° C depression in Central Europe. Afterwards it has been discussed whether or not these relatively small depressions can be explained exclusively on the basis of the higher continentality of the central part of Eurasia in comparison with the western or eastern part of this continent. As this seems to be impossible, it is necessary to look for other facts that could be related to this problem. In the opinion of the author the relative stability of climatic conditions in Western Siberia during the whole Quaternary could be easily explained by the change between the meridional-circulation (low-index-type), prevailing during the glacial periods, and the reinforced zonal-circulation (high-index-type) during the interglacial and postglacial periods. Article in Journal/Newspaper Arctic Tundra Siberia Niedersächsisches Online-Archiv NOA Arctic E&G Quaternary Science Journal 11 1 77 87 |
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Niedersächsisches Online-Archiv NOA |
op_collection_id |
ftnonlinearchiv |
language |
English |
topic |
article Verlagsveröffentlichung |
spellingShingle |
article Verlagsveröffentlichung Weischet, W. Zum Problem der Stabilität der Klimabedingungen in Westsibirien während der Glaziale und Interglaziale |
topic_facet |
article Verlagsveröffentlichung |
description |
The depression values of the summer temperature and also of the mean annual temperature in Western Siberia during the last glaciation, have been deduced. This calculation has been based on the different position of the boreal boundaries of the tundra and the continental deciduous forests during the ice ages and at the present time. According to these calculations the following depressions of summer temperature have been obtained: 5-8° C near the arctic circle and 2-4° C in the latitude of 50° North, in comparison with the 10-12° C depression in Central Europe. Afterwards it has been discussed whether or not these relatively small depressions can be explained exclusively on the basis of the higher continentality of the central part of Eurasia in comparison with the western or eastern part of this continent. As this seems to be impossible, it is necessary to look for other facts that could be related to this problem. In the opinion of the author the relative stability of climatic conditions in Western Siberia during the whole Quaternary could be easily explained by the change between the meridional-circulation (low-index-type), prevailing during the glacial periods, and the reinforced zonal-circulation (high-index-type) during the interglacial and postglacial periods. |
format |
Article in Journal/Newspaper |
author |
Weischet, W. |
author_facet |
Weischet, W. |
author_sort |
Weischet, W. |
title |
Zum Problem der Stabilität der Klimabedingungen in Westsibirien während der Glaziale und Interglaziale |
title_short |
Zum Problem der Stabilität der Klimabedingungen in Westsibirien während der Glaziale und Interglaziale |
title_full |
Zum Problem der Stabilität der Klimabedingungen in Westsibirien während der Glaziale und Interglaziale |
title_fullStr |
Zum Problem der Stabilität der Klimabedingungen in Westsibirien während der Glaziale und Interglaziale |
title_full_unstemmed |
Zum Problem der Stabilität der Klimabedingungen in Westsibirien während der Glaziale und Interglaziale |
title_sort |
zum problem der stabilität der klimabedingungen in westsibirien während der glaziale und interglaziale |
publisher |
Geozon Science Media |
publishDate |
1960 |
url |
https://doi.org/10.3285/eg.11.1.09 https://noa.gwlb.de/receive/cop_mods_00039725 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00039402/egqsj-11-77-1960.pdf https://egqsj.copernicus.org/articles/11/77/1960/egqsj-11-77-1960.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Tundra Siberia |
genre_facet |
Arctic Tundra Siberia |
op_relation |
E&G Quaternary Science Journal -- Quaternary science journal -- http://www.bibliothek.uni-regensburg.de/ezeit/?2572732 -- https://www.eg-quaternary-sci-j.net/volumes.html -- 2199-9090 https://doi.org/10.3285/eg.11.1.09 https://noa.gwlb.de/receive/cop_mods_00039725 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00039402/egqsj-11-77-1960.pdf https://egqsj.copernicus.org/articles/11/77/1960/egqsj-11-77-1960.pdf |
op_rights |
uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.3285/eg.11.1.09 |
container_title |
E&G Quaternary Science Journal |
container_volume |
11 |
container_issue |
1 |
container_start_page |
77 |
op_container_end_page |
87 |
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1766339247879487488 |