Link of volcanic activity and climate change in Altai studied in the ice core from Belukha Mountain

In the present research we discuss a role of volcanic activity in Altai thermal regime. Here we analyses the sulfate and temperature data reconstructed from the natural paleoarchive – ice core from the Belukha Mountain saddle. Sulfate ice-core reconstructions can serve as volcanic markers. The both ...

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Main Authors: N. S. Malygina, T. V. Barlyaeva, T. S. Papina
Format: Article
Language:Russian
Published: Nauka 2015-04-01
Series:Lëd i Sneg
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/107
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spelling doaj-9e3a7c06c5994caaa79a669970d4247c2021-08-02T08:42:07ZrusNaukaLëd i Sneg2076-67342412-37652015-04-0153211212010.15356/2076-6734-2013-2-112-120101Link of volcanic activity and climate change in Altai studied in the ice core from Belukha MountainN. S. Malygina0T. V. Barlyaeva1T. S. Papina2Institute of Water and Ecological Problems, Siberian Branch of RAS, Barnaul;European Center of Study and Education in the Earth Sciences and Environment, Provence, FranceInstitute of Water and Ecological Problems, Siberian Branch of RAS, Barnaul;In the present research we discuss a role of volcanic activity in Altai thermal regime. Here we analyses the sulfate and temperature data reconstructed from the natural paleoarchive – ice core from the Belukha Mountain saddle. Sulfate ice-core reconstructions can serve as volcanic markers. The both – sulfate and temperature reconstructions – are for the last 750 years. As the characteristic of volcanic activity we consider Volcanic Explosivity Index (VEI), Dust Veil Index (DVI) and Ice core volcanic index (IVI). The analysis was done using wavelet analysis and analysis of wavelet cross coherence and phase. As the result, we conclude that observed increases in the values of the indexes VEI, DVI, IVI basically correspond to decreases of temperature and increases of sulfate concentrations. This confirms the dependence of changes in the thermal regime of the Altai from volcanic activity. But in the 1750–1850 years period there is a delay of the changes in temperature with respect to the changes in volcanic activity. We suggest that it can be due to the superposition of the influence of solar and volcanic activity on changes in the thermal regime of Altai.https://ice-snow.igras.ru/jour/article/view/107altaiclimate changeice corevolcanic eruptions.
collection DOAJ
language Russian
format Article
sources DOAJ
author N. S. Malygina
T. V. Barlyaeva
T. S. Papina
spellingShingle N. S. Malygina
T. V. Barlyaeva
T. S. Papina
Link of volcanic activity and climate change in Altai studied in the ice core from Belukha Mountain
Lëd i Sneg
altai
climate change
ice core
volcanic eruptions.
author_facet N. S. Malygina
T. V. Barlyaeva
T. S. Papina
author_sort N. S. Malygina
title Link of volcanic activity and climate change in Altai studied in the ice core from Belukha Mountain
title_short Link of volcanic activity and climate change in Altai studied in the ice core from Belukha Mountain
title_full Link of volcanic activity and climate change in Altai studied in the ice core from Belukha Mountain
title_fullStr Link of volcanic activity and climate change in Altai studied in the ice core from Belukha Mountain
title_full_unstemmed Link of volcanic activity and climate change in Altai studied in the ice core from Belukha Mountain
title_sort link of volcanic activity and climate change in altai studied in the ice core from belukha mountain
publisher Nauka
series Lëd i Sneg
issn 2076-6734
2412-3765
publishDate 2015-04-01
description In the present research we discuss a role of volcanic activity in Altai thermal regime. Here we analyses the sulfate and temperature data reconstructed from the natural paleoarchive – ice core from the Belukha Mountain saddle. Sulfate ice-core reconstructions can serve as volcanic markers. The both – sulfate and temperature reconstructions – are for the last 750 years. As the characteristic of volcanic activity we consider Volcanic Explosivity Index (VEI), Dust Veil Index (DVI) and Ice core volcanic index (IVI). The analysis was done using wavelet analysis and analysis of wavelet cross coherence and phase. As the result, we conclude that observed increases in the values of the indexes VEI, DVI, IVI basically correspond to decreases of temperature and increases of sulfate concentrations. This confirms the dependence of changes in the thermal regime of the Altai from volcanic activity. But in the 1750–1850 years period there is a delay of the changes in temperature with respect to the changes in volcanic activity. We suggest that it can be due to the superposition of the influence of solar and volcanic activity on changes in the thermal regime of Altai.
topic altai
climate change
ice core
volcanic eruptions.
url https://ice-snow.igras.ru/jour/article/view/107
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