A link between an ice age era and a rapid polar shift
The striking asymmetry of the ice cover during the Last Global Maximum suggests that the North Pole was in Greenland and then rapidly shifted to its present position in the Arctic See. A scenario which causes such a rapid geographic polar shift is physically possible. It involves an additional plane...
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Online Access: | https://dx.doi.org/10.48550/arxiv.physics/0407082 https://arxiv.org/abs/physics/0407082 |
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ftdatacite:10.48550/arxiv.physics/0407082 2023-05-15T15:01:13+02:00 A link between an ice age era and a rapid polar shift Woelfli, W. Baltensperger, W. 2004 https://dx.doi.org/10.48550/arxiv.physics/0407082 https://arxiv.org/abs/physics/0407082 unknown arXiv Assumed arXiv.org perpetual, non-exclusive license to distribute this article for submissions made before January 2004 http://arxiv.org/licenses/assumed-1991-2003/ Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences Preprint Article article CreativeWork 2004 ftdatacite https://doi.org/10.48550/arxiv.physics/0407082 2022-04-01T16:18:05Z The striking asymmetry of the ice cover during the Last Global Maximum suggests that the North Pole was in Greenland and then rapidly shifted to its present position in the Arctic See. A scenario which causes such a rapid geographic polar shift is physically possible. It involves an additional planet, which disappeared by evaporation within the Holocene. This is only possible within such a short period, if the planet was in an extremely eccentric orbit and hot. Then, since this produced an interplanetary gas cloud, the polar shift had to be preceded by a cold period with large global temperature variations during several million years. : 4 pages Report Arctic Greenland North Pole DataCite Metadata Store (German National Library of Science and Technology) Arctic Greenland North Pole |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences |
spellingShingle |
Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences Woelfli, W. Baltensperger, W. A link between an ice age era and a rapid polar shift |
topic_facet |
Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences |
description |
The striking asymmetry of the ice cover during the Last Global Maximum suggests that the North Pole was in Greenland and then rapidly shifted to its present position in the Arctic See. A scenario which causes such a rapid geographic polar shift is physically possible. It involves an additional planet, which disappeared by evaporation within the Holocene. This is only possible within such a short period, if the planet was in an extremely eccentric orbit and hot. Then, since this produced an interplanetary gas cloud, the polar shift had to be preceded by a cold period with large global temperature variations during several million years. : 4 pages |
format |
Report |
author |
Woelfli, W. Baltensperger, W. |
author_facet |
Woelfli, W. Baltensperger, W. |
author_sort |
Woelfli, W. |
title |
A link between an ice age era and a rapid polar shift |
title_short |
A link between an ice age era and a rapid polar shift |
title_full |
A link between an ice age era and a rapid polar shift |
title_fullStr |
A link between an ice age era and a rapid polar shift |
title_full_unstemmed |
A link between an ice age era and a rapid polar shift |
title_sort |
link between an ice age era and a rapid polar shift |
publisher |
arXiv |
publishDate |
2004 |
url |
https://dx.doi.org/10.48550/arxiv.physics/0407082 https://arxiv.org/abs/physics/0407082 |
geographic |
Arctic Greenland North Pole |
geographic_facet |
Arctic Greenland North Pole |
genre |
Arctic Greenland North Pole |
genre_facet |
Arctic Greenland North Pole |
op_rights |
Assumed arXiv.org perpetual, non-exclusive license to distribute this article for submissions made before January 2004 http://arxiv.org/licenses/assumed-1991-2003/ |
op_doi |
https://doi.org/10.48550/arxiv.physics/0407082 |
_version_ |
1766333246949294080 |