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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Bibliographic Details
Main Author: Mikhail V. Kabanov
Format: Article in Journal/Newspaper
Language:English
Russian
Published: Siberian Federal University 2008
Subjects:
Online Access:https://doaj.org/article/2f485b19a87c497ba6a6c0ff3654d9d7
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spelling 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
institution 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
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