Some Regularities in Climatic and Ecosystem Changes in Siberia
Applying statistical analysis to instrumented data accumulated in the world meteorological network, we revealed regularities of climatic and ecosystems changes observed in Siberian region. It was shown that warming, observed in Siberia over last climatic period (30 years), is characterized by inhomo...
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Siberian Federal University
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ftdoajarticles:oai:doaj.org/article:2f485b19a87c497ba6a6c0ff3654d9d7 2023-05-15T17:33:18+02:00 Some Regularities in Climatic and Ecosystem Changes in Siberia Mikhail V. Kabanov 2008-12-01T00:00:00Z https://doaj.org/article/2f485b19a87c497ba6a6c0ff3654d9d7 EN RU eng rus Siberian Federal University http://elib.sfu-kras.ru/bitstream/2311/942/3/01_%d0%9a%d0%b0%d0%b1%d0%b0%d0%bd%d0%be%d0%b2.pdf https://doaj.org/toc/1997-1389 https://doaj.org/toc/2313-5530 1997-1389 2313-5530 https://doaj.org/article/2f485b19a87c497ba6a6c0ff3654d9d7 Журнал Сибирского федерального университета: Серия Биология, Vol 1, Iss 4, Pp 312-322 (2008) climate changes ecosystem changes warming map wavelet analysis great vasyugan bog Biotechnology TP248.13-248.65 Biology (General) QH301-705.5 article 2008 ftdoajarticles 2022-12-31T01:29:45Z Applying statistical analysis to instrumented data accumulated in the world meteorological network, we revealed regularities of climatic and ecosystems changes observed in Siberian region. It was shown that warming, observed in Siberia over last climatic period (30 years), is characterized by inhomogeneous subregional structure with mesoscale spots having accelerated warming rates up to 0.5 °С/10 years. Trends of surface pressure for the same period have lesser contrast subregional structure with decrease of annual mean pressure down to 0.2-0.4 hPa/10 years. Wavelet analysis applied to time variability of climatic parameters over the past century found out periodicities with the scales of 10-12 and 30-50 years. Comparing wavelet spectra of surface temperature in West Siberia and North-Atlantic Oscillation index, we revealed their correlation in 1940-1990 with time shift up to 7 years. This climatic phenomenon could be explained by possible inertia mechanisms in oceanic heat transfer. Based on results of ground and airborne and spaceborne instrumented observations, we discuss climatic influence of Siberian bogs (using Great Vasyugan Bog as an example). Article in Journal/Newspaper North Atlantic North Atlantic oscillation Siberia Directory of Open Access Journals: DOAJ Articles |
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Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English Russian |
topic |
climate changes ecosystem changes warming map wavelet analysis great vasyugan bog Biotechnology TP248.13-248.65 Biology (General) QH301-705.5 |
spellingShingle |
climate changes ecosystem changes warming map wavelet analysis great vasyugan bog Biotechnology TP248.13-248.65 Biology (General) QH301-705.5 Mikhail V. Kabanov Some Regularities in Climatic and Ecosystem Changes in Siberia |
topic_facet |
climate changes ecosystem changes warming map wavelet analysis great vasyugan bog Biotechnology TP248.13-248.65 Biology (General) QH301-705.5 |
description |
Applying statistical analysis to instrumented data accumulated in the world meteorological network, we revealed regularities of climatic and ecosystems changes observed in Siberian region. It was shown that warming, observed in Siberia over last climatic period (30 years), is characterized by inhomogeneous subregional structure with mesoscale spots having accelerated warming rates up to 0.5 °С/10 years. Trends of surface pressure for the same period have lesser contrast subregional structure with decrease of annual mean pressure down to 0.2-0.4 hPa/10 years. Wavelet analysis applied to time variability of climatic parameters over the past century found out periodicities with the scales of 10-12 and 30-50 years. Comparing wavelet spectra of surface temperature in West Siberia and North-Atlantic Oscillation index, we revealed their correlation in 1940-1990 with time shift up to 7 years. This climatic phenomenon could be explained by possible inertia mechanisms in oceanic heat transfer. Based on results of ground and airborne and spaceborne instrumented observations, we discuss climatic influence of Siberian bogs (using Great Vasyugan Bog as an example). |
format |
Article in Journal/Newspaper |
author |
Mikhail V. Kabanov |
author_facet |
Mikhail V. Kabanov |
author_sort |
Mikhail V. Kabanov |
title |
Some Regularities in Climatic and Ecosystem Changes in Siberia |
title_short |
Some Regularities in Climatic and Ecosystem Changes in Siberia |
title_full |
Some Regularities in Climatic and Ecosystem Changes in Siberia |
title_fullStr |
Some Regularities in Climatic and Ecosystem Changes in Siberia |
title_full_unstemmed |
Some Regularities in Climatic and Ecosystem Changes in Siberia |
title_sort |
some regularities in climatic and ecosystem changes in siberia |
publisher |
Siberian Federal University |
publishDate |
2008 |
url |
https://doaj.org/article/2f485b19a87c497ba6a6c0ff3654d9d7 |
genre |
North Atlantic North Atlantic oscillation Siberia |
genre_facet |
North Atlantic North Atlantic oscillation Siberia |
op_source |
Журнал Сибирского федерального университета: Серия Биология, Vol 1, Iss 4, Pp 312-322 (2008) |
op_relation |
http://elib.sfu-kras.ru/bitstream/2311/942/3/01_%d0%9a%d0%b0%d0%b1%d0%b0%d0%bd%d0%be%d0%b2.pdf https://doaj.org/toc/1997-1389 https://doaj.org/toc/2313-5530 1997-1389 2313-5530 https://doaj.org/article/2f485b19a87c497ba6a6c0ff3654d9d7 |
_version_ |
1766131769379127296 |