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...
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Language: | German English |
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Copernicus Publications
1960
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ftdoajarticles:oai:doaj.org/article:d51594fc88f94fcb879b43cd16b3a524 2023-05-15T15:07:25+02:00 Zum Problem der Stabilität der Klimabedingungen in Westsibirien während der Glaziale und Interglaziale W. Weischet 1960-12-01T00:00:00Z https://doi.org/10.3285/eg.11.1.09 https://doaj.org/article/d51594fc88f94fcb879b43cd16b3a524 DE EN ger eng Copernicus Publications https://www.eg-quaternary-sci-j.net/11/77/1960/egqsj-11-77-1960.pdf https://doaj.org/toc/0424-7116 https://doaj.org/toc/2199-9090 doi:10.3285/eg.11.1.09 0424-7116 2199-9090 https://doaj.org/article/d51594fc88f94fcb879b43cd16b3a524 Eiszeitalter und Gegenwart, Vol 11, Pp 77-87 (1960) Geology QE1-996.5 article 1960 ftdoajarticles https://doi.org/10.3285/eg.11.1.09 2022-12-31T08:54:02Z 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 Directory of Open Access Journals: DOAJ Articles Arctic E&G Quaternary Science Journal 11 1 77 87 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
German English |
topic |
Geology QE1-996.5 |
spellingShingle |
Geology QE1-996.5 W. Weischet Zum Problem der Stabilität der Klimabedingungen in Westsibirien während der Glaziale und Interglaziale |
topic_facet |
Geology QE1-996.5 |
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 |
W. Weischet |
author_facet |
W. Weischet |
author_sort |
W. Weischet |
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 |
Copernicus Publications |
publishDate |
1960 |
url |
https://doi.org/10.3285/eg.11.1.09 https://doaj.org/article/d51594fc88f94fcb879b43cd16b3a524 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Tundra Siberia |
genre_facet |
Arctic Tundra Siberia |
op_source |
Eiszeitalter und Gegenwart, Vol 11, Pp 77-87 (1960) |
op_relation |
https://www.eg-quaternary-sci-j.net/11/77/1960/egqsj-11-77-1960.pdf https://doaj.org/toc/0424-7116 https://doaj.org/toc/2199-9090 doi:10.3285/eg.11.1.09 0424-7116 2199-9090 https://doaj.org/article/d51594fc88f94fcb879b43cd16b3a524 |
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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1766338927604531200 |