Modeling the influence of the Earth rotation axis position on the global climate variations

Abstract This study presents the results of numerical experiments to determine the Earth’s climate when its rotation axis is displaced without changing the axis tilt to the ecliptic plane. There is some evidence of the possibility of this shift in the past. The calculations were carried out using a...

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Published in:Journal of Physics: Conference Series
Main Author: Parkhomenko, V P
Format: Article in Journal/Newspaper
Language:unknown
Published: IOP Publishing 2021
Subjects:
Online Access:http://dx.doi.org/10.1088/1742-6596/1730/1/012072
https://iopscience.iop.org/article/10.1088/1742-6596/1730/1/012072
https://iopscience.iop.org/article/10.1088/1742-6596/1730/1/012072/pdf
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spelling crioppubl:10.1088/1742-6596/1730/1/012072 2024-06-02T07:57:55+00:00 Modeling the influence of the Earth rotation axis position on the global climate variations Parkhomenko, V P 2021 http://dx.doi.org/10.1088/1742-6596/1730/1/012072 https://iopscience.iop.org/article/10.1088/1742-6596/1730/1/012072 https://iopscience.iop.org/article/10.1088/1742-6596/1730/1/012072/pdf unknown IOP Publishing http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining Journal of Physics: Conference Series volume 1730, issue 1, page 012072 ISSN 1742-6588 1742-6596 journal-article 2021 crioppubl https://doi.org/10.1088/1742-6596/1730/1/012072 2024-05-07T13:54:59Z Abstract This study presents the results of numerical experiments to determine the Earth’s climate when its rotation axis is displaced without changing the axis tilt to the ecliptic plane. There is some evidence of the possibility of this shift in the past. The calculations were carried out using a hydrodynamic three-dimensional global climate model, including blocks of atmosphere, thermohaline large-scale ocean circulation and sea ice. Numerical experiments demonstrate a significant temperature changes throughout the world. A large area of Antarctica warmed up to temperatures above 15 ° C. This is reason of intense melting of glaciers for a long time. Significant warming of the Arctic Ocean will lead to sea ice melting in the Arctic. Strong changes in temperature and ice cover lead to significant changes in horizontal ocean circulation. A procedure is proposed for calculating wind speed in atmosphere energy - moisture balance model. It is based on the geostrophic approach, taking into account the thermal component of the wind, and introducing the mechanism of friction on the underlying surface. A technique has been developed for the formation of the necessary maps and the relationships between them when turning the Earth rotation axis or using new cartographic data. Article in Journal/Newspaper Antarc* Antarctica Arctic Arctic Ocean Sea ice IOP Publishing Arctic Arctic Ocean Journal of Physics: Conference Series 1730 1 012072
institution Open Polar
collection IOP Publishing
op_collection_id crioppubl
language unknown
description Abstract This study presents the results of numerical experiments to determine the Earth’s climate when its rotation axis is displaced without changing the axis tilt to the ecliptic plane. There is some evidence of the possibility of this shift in the past. The calculations were carried out using a hydrodynamic three-dimensional global climate model, including blocks of atmosphere, thermohaline large-scale ocean circulation and sea ice. Numerical experiments demonstrate a significant temperature changes throughout the world. A large area of Antarctica warmed up to temperatures above 15 ° C. This is reason of intense melting of glaciers for a long time. Significant warming of the Arctic Ocean will lead to sea ice melting in the Arctic. Strong changes in temperature and ice cover lead to significant changes in horizontal ocean circulation. A procedure is proposed for calculating wind speed in atmosphere energy - moisture balance model. It is based on the geostrophic approach, taking into account the thermal component of the wind, and introducing the mechanism of friction on the underlying surface. A technique has been developed for the formation of the necessary maps and the relationships between them when turning the Earth rotation axis or using new cartographic data.
format Article in Journal/Newspaper
author Parkhomenko, V P
spellingShingle Parkhomenko, V P
Modeling the influence of the Earth rotation axis position on the global climate variations
author_facet Parkhomenko, V P
author_sort Parkhomenko, V P
title Modeling the influence of the Earth rotation axis position on the global climate variations
title_short Modeling the influence of the Earth rotation axis position on the global climate variations
title_full Modeling the influence of the Earth rotation axis position on the global climate variations
title_fullStr Modeling the influence of the Earth rotation axis position on the global climate variations
title_full_unstemmed Modeling the influence of the Earth rotation axis position on the global climate variations
title_sort modeling the influence of the earth rotation axis position on the global climate variations
publisher IOP Publishing
publishDate 2021
url http://dx.doi.org/10.1088/1742-6596/1730/1/012072
https://iopscience.iop.org/article/10.1088/1742-6596/1730/1/012072
https://iopscience.iop.org/article/10.1088/1742-6596/1730/1/012072/pdf
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Antarc*
Antarctica
Arctic
Arctic Ocean
Sea ice
genre_facet Antarc*
Antarctica
Arctic
Arctic Ocean
Sea ice
op_source Journal of Physics: Conference Series
volume 1730, issue 1, page 012072
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_doi https://doi.org/10.1088/1742-6596/1730/1/012072
container_title Journal of Physics: Conference Series
container_volume 1730
container_issue 1
container_start_page 012072
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