The nature of the storm activity in the northwest Atlantic during the Holocene and its possible connection with variations in the Earth’s magnetic field
Abstract The data on the concentration of ions in the core of the Greenland Ice Sheet Project 2 (GISP2) were analysed to find the cause of storm activity in the north-west Atlantic during the Holocene. It was shown that there is cyclical transfer of ionic components with a period of ∼ 2700 years due...
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crioppubl:10.1088/1742-6596/1697/1/012010 2023-05-15T16:19:38+02:00 The nature of the storm activity in the northwest Atlantic during the Holocene and its possible connection with variations in the Earth’s magnetic field Vasiliev, S S Dergachev, V A 2020 http://dx.doi.org/10.1088/1742-6596/1697/1/012010 https://iopscience.iop.org/article/10.1088/1742-6596/1697/1/012010/pdf https://iopscience.iop.org/article/10.1088/1742-6596/1697/1/012010 unknown IOP Publishing http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining CC-BY Journal of Physics: Conference Series volume 1697, issue 1, page 012010 ISSN 1742-6588 1742-6596 General Physics and Astronomy journal-article 2020 crioppubl https://doi.org/10.1088/1742-6596/1697/1/012010 2022-04-25T05:18:03Z Abstract The data on the concentration of ions in the core of the Greenland Ice Sheet Project 2 (GISP2) were analysed to find the cause of storm activity in the north-west Atlantic during the Holocene. It was shown that there is cyclical transfer of ionic components with a period of ∼ 2700 years due to changes in storm activity. As a possible cause of storm changes, secular variations in the position of the geomagnetic pole over the past several thousand years have been considered. In particular, the periodicity of fluctuations in the longitude of the north geomagnetic pole was compared with the frequency of intensification of storm activity. It has been demonstrated that the spectra of these variations are similar, from which it is concluded that secular variations in the magnetic field are the basis of the processes that determine the variability of storm activity and climate in the north-west Atlantic during the Holocene. Article in Journal/Newspaper Geomagnetic Pole Greenland Greenland Ice Sheet Project Ice Sheet North West Atlantic Northwest Atlantic IOP Publishing (via Crossref) Greenland Journal of Physics: Conference Series 1697 012010 |
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IOP Publishing (via Crossref) |
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unknown |
topic |
General Physics and Astronomy |
spellingShingle |
General Physics and Astronomy Vasiliev, S S Dergachev, V A The nature of the storm activity in the northwest Atlantic during the Holocene and its possible connection with variations in the Earth’s magnetic field |
topic_facet |
General Physics and Astronomy |
description |
Abstract The data on the concentration of ions in the core of the Greenland Ice Sheet Project 2 (GISP2) were analysed to find the cause of storm activity in the north-west Atlantic during the Holocene. It was shown that there is cyclical transfer of ionic components with a period of ∼ 2700 years due to changes in storm activity. As a possible cause of storm changes, secular variations in the position of the geomagnetic pole over the past several thousand years have been considered. In particular, the periodicity of fluctuations in the longitude of the north geomagnetic pole was compared with the frequency of intensification of storm activity. It has been demonstrated that the spectra of these variations are similar, from which it is concluded that secular variations in the magnetic field are the basis of the processes that determine the variability of storm activity and climate in the north-west Atlantic during the Holocene. |
format |
Article in Journal/Newspaper |
author |
Vasiliev, S S Dergachev, V A |
author_facet |
Vasiliev, S S Dergachev, V A |
author_sort |
Vasiliev, S S |
title |
The nature of the storm activity in the northwest Atlantic during the Holocene and its possible connection with variations in the Earth’s magnetic field |
title_short |
The nature of the storm activity in the northwest Atlantic during the Holocene and its possible connection with variations in the Earth’s magnetic field |
title_full |
The nature of the storm activity in the northwest Atlantic during the Holocene and its possible connection with variations in the Earth’s magnetic field |
title_fullStr |
The nature of the storm activity in the northwest Atlantic during the Holocene and its possible connection with variations in the Earth’s magnetic field |
title_full_unstemmed |
The nature of the storm activity in the northwest Atlantic during the Holocene and its possible connection with variations in the Earth’s magnetic field |
title_sort |
nature of the storm activity in the northwest atlantic during the holocene and its possible connection with variations in the earth’s magnetic field |
publisher |
IOP Publishing |
publishDate |
2020 |
url |
http://dx.doi.org/10.1088/1742-6596/1697/1/012010 https://iopscience.iop.org/article/10.1088/1742-6596/1697/1/012010/pdf https://iopscience.iop.org/article/10.1088/1742-6596/1697/1/012010 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Geomagnetic Pole Greenland Greenland Ice Sheet Project Ice Sheet North West Atlantic Northwest Atlantic |
genre_facet |
Geomagnetic Pole Greenland Greenland Ice Sheet Project Ice Sheet North West Atlantic Northwest Atlantic |
op_source |
Journal of Physics: Conference Series volume 1697, issue 1, page 012010 ISSN 1742-6588 1742-6596 |
op_rights |
http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1088/1742-6596/1697/1/012010 |
container_title |
Journal of Physics: Conference Series |
container_volume |
1697 |
container_start_page |
012010 |
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1766006046426398720 |