A modern interpretation of the history of the Pleistocene glacial cycles
One of the, Glaciological descriptions of Greenland and Antarctica were among the most outstanding events in the geographical investigations of the Earth, made in the 20th century. They have shown that glaciations, traces of which were found in Europe and North America in the first half of the 19th...
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ftdoajarticles:oai:doaj.org/article:6c765f17b3434678a38e5c243c47ae9b 2023-05-15T14:04:02+02:00 A modern interpretation of the history of the Pleistocene glacial cycles V. M. Kotlyakov D. M. Sonechkin 2015-05-01T00:00:00Z https://doi.org/10.15356/2076-6734-2015-2-103-122 https://doaj.org/article/6c765f17b3434678a38e5c243c47ae9b RU rus Nauka https://ice-snow.igras.ru/jour/article/view/173 https://doaj.org/toc/2076-6734 https://doaj.org/toc/2412-3765 2076-6734 2412-3765 doi:10.15356/2076-6734-2015-2-103-122 https://doaj.org/article/6c765f17b3434678a38e5c243c47ae9b Лëд и снег, Vol 55, Iss 2, Pp 103-122 (2015) ледниковые циклы плейстоцена теория миланковича теория нелинейных динамических систем странный нехаотический аттрактор Science Q article 2015 ftdoajarticles https://doi.org/10.15356/2076-6734-2015-2-103-122 2023-03-19T01:40:13Z One of the, Glaciological descriptions of Greenland and Antarctica were among the most outstanding events in the geographical investigations of the Earth, made in the 20th century. They have shown that glaciations, traces of which were found in Europe and North America in the first half of the 19th century, waxed and waned during the Pleistocene repeatedly and were synchronous with the expansions and reductions of the Antarctic ice sheet. Further analyses of the sea-bed sediments confirmed the fact of such synchronicity, and revealed that the durations of the Pleistocene glacial cycles (on the order of one hundred thousand years) were significantly longer then approximately forty thousand years alternations of the warm and cold climate conditions during the preceding Pliocene. In this paper, using wavelets, and methods of the theory of the nonlinear dynamical systems, patterns of the Pleistocene’s and Pliocene’s cyclic variations of climate are compared with each other, to understand the mechanisms which can be responsible for their excitation and evolution. Article in Journal/Newspaper Antarc* Antarctic Antarctica Greenland Ice Sheet Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic Greenland Ice and Snow 130 2 103 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
Russian |
topic |
ледниковые циклы плейстоцена теория миланковича теория нелинейных динамических систем странный нехаотический аттрактор Science Q |
spellingShingle |
ледниковые циклы плейстоцена теория миланковича теория нелинейных динамических систем странный нехаотический аттрактор Science Q V. M. Kotlyakov D. M. Sonechkin A modern interpretation of the history of the Pleistocene glacial cycles |
topic_facet |
ледниковые циклы плейстоцена теория миланковича теория нелинейных динамических систем странный нехаотический аттрактор Science Q |
description |
One of the, Glaciological descriptions of Greenland and Antarctica were among the most outstanding events in the geographical investigations of the Earth, made in the 20th century. They have shown that glaciations, traces of which were found in Europe and North America in the first half of the 19th century, waxed and waned during the Pleistocene repeatedly and were synchronous with the expansions and reductions of the Antarctic ice sheet. Further analyses of the sea-bed sediments confirmed the fact of such synchronicity, and revealed that the durations of the Pleistocene glacial cycles (on the order of one hundred thousand years) were significantly longer then approximately forty thousand years alternations of the warm and cold climate conditions during the preceding Pliocene. In this paper, using wavelets, and methods of the theory of the nonlinear dynamical systems, patterns of the Pleistocene’s and Pliocene’s cyclic variations of climate are compared with each other, to understand the mechanisms which can be responsible for their excitation and evolution. |
format |
Article in Journal/Newspaper |
author |
V. M. Kotlyakov D. M. Sonechkin |
author_facet |
V. M. Kotlyakov D. M. Sonechkin |
author_sort |
V. M. Kotlyakov |
title |
A modern interpretation of the history of the Pleistocene glacial cycles |
title_short |
A modern interpretation of the history of the Pleistocene glacial cycles |
title_full |
A modern interpretation of the history of the Pleistocene glacial cycles |
title_fullStr |
A modern interpretation of the history of the Pleistocene glacial cycles |
title_full_unstemmed |
A modern interpretation of the history of the Pleistocene glacial cycles |
title_sort |
modern interpretation of the history of the pleistocene glacial cycles |
publisher |
Nauka |
publishDate |
2015 |
url |
https://doi.org/10.15356/2076-6734-2015-2-103-122 https://doaj.org/article/6c765f17b3434678a38e5c243c47ae9b |
geographic |
Antarctic The Antarctic Greenland |
geographic_facet |
Antarctic The Antarctic Greenland |
genre |
Antarc* Antarctic Antarctica Greenland Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica Greenland Ice Sheet |
op_source |
Лëд и снег, Vol 55, Iss 2, Pp 103-122 (2015) |
op_relation |
https://ice-snow.igras.ru/jour/article/view/173 https://doaj.org/toc/2076-6734 https://doaj.org/toc/2412-3765 2076-6734 2412-3765 doi:10.15356/2076-6734-2015-2-103-122 https://doaj.org/article/6c765f17b3434678a38e5c243c47ae9b |
op_doi |
https://doi.org/10.15356/2076-6734-2015-2-103-122 |
container_title |
Ice and Snow |
container_volume |
130 |
container_issue |
2 |
container_start_page |
103 |
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1766274975450267648 |