History of sea ice in the Arctic basin: Lessons from the past for future

The process of the sea ice formation in the Arctic Ocean is analyzed for the period of the last 65 million years, i.e. from the Paleocene to the present time. Appearance of sea ice in the high latitudes is demonstrated to be caused by the negative trend in global temperatures due to decreasing of th...

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Published in:Ice and Snow
Main Authors: I. Borzenkova I., И. Борзенкова И.
Format: Article in Journal/Newspaper
Language:Russian
Published: IGRAS 2016
Subjects:
Arctic
current global warming
history of sea icing
last 65 million years
sea ice
the Cenozoic time
история образования морских льдов;кайнозой;морские льды;последние 65 млн лет;современное глобальное потепление
Arctic Ocean
albedo
Arctic Basin
Global warming
Sea ice
Online Access:https://ice-snow.igras.ru/jour/article/view/301
https://doi.org/10.15356/2076-6734-2016-2-221-234
id ftjias:oai:oai.ice.elpub.ru:article/301
record_format openpolar
institution Open Polar
collection Ice and Snow (E-Journal)
op_collection_id ftjias
language Russian
topic Arctic
current global warming
history of sea icing
last 65 million years
sea ice
the Cenozoic time
история образования морских льдов;кайнозой;морские льды;последние 65 млн лет;современное глобальное потепление
spellingShingle Arctic
current global warming
history of sea icing
last 65 million years
sea ice
the Cenozoic time
история образования морских льдов;кайнозой;морские льды;последние 65 млн лет;современное глобальное потепление
I. Borzenkova I.
И. Борзенкова И.
History of sea ice in the Arctic basin: Lessons from the past for future
topic_facet Arctic
current global warming
history of sea icing
last 65 million years
sea ice
the Cenozoic time
история образования морских льдов;кайнозой;морские льды;последние 65 млн лет;современное глобальное потепление
description The process of the sea ice formation in the Arctic Ocean is analyzed for the period of the last 65 million years, i.e. from the Paleocene to the present time. Appearance of sea ice in the high latitudes is demonstrated to be caused by the negative trend in global temperatures due to decreasing of the CO2 concentration in the ancient atmosphere. Formation of seasonal and perennial ice cover in the limited area near the Pole could take place during the mid-Neogene period, about 12–13 Ma ago. However, areas of the sea icing could be obviously changed for this time during periods of the climate warming and cooling. Permanent sea ice had been formed in the early Pleistocene, i.e. about 2.0–1.8 Ma ago only. Paleoclimatic reconstructions, based on the indirect data and modeling simulation for the Holocene optimum (10–6 ka ago) and for the Last Interglacial period (the isotopic substage in the marine cross-section 5e, about 125–127 ka ago) had shown that rising of global temperatures by 1.0–1.5 °C resulted in strong decreasing of the sea ice area, and the perennial ice cover became the seasonal one. Relatively small changes in the incoming solar radiation originating during the spring-summer time due to the orbital factors played the role of a trigger for onset of the melting process. Further on, the process could be enhanced owing to difference in the albedo between the ice cover and open water. Recently, the rapid shortening of the sea ice area is noted, and in some parts of the Arctic Ocean the area is twice cut down as compared with the normal. In 2015, the record low area of the winter sea ice was observed, and therewith the maximum of the ice area shifted to the earlier period (by 15 days) as compared with the period of 1981–2010. The winter fluctuations of the sea ice areas are as much important as the summer ones, since they are the best indicators of the present-day global warming. Thus, it can be supposed that some mechanism of replacing the perennial sea ice by the seasonal ones has been started up, that is ...
format Article in Journal/Newspaper
author I. Borzenkova I.
И. Борзенкова И.
author_facet I. Borzenkova I.
И. Борзенкова И.
author_sort I. Borzenkova I.
title History of sea ice in the Arctic basin: Lessons from the past for future
title_short History of sea ice in the Arctic basin: Lessons from the past for future
title_full History of sea ice in the Arctic basin: Lessons from the past for future
title_fullStr History of sea ice in the Arctic basin: Lessons from the past for future
title_full_unstemmed History of sea ice in the Arctic basin: Lessons from the past for future
title_sort history of sea ice in the arctic basin: lessons from the past for future
publisher IGRAS
publishDate 2016
url https://ice-snow.igras.ru/jour/article/view/301
https://doi.org/10.15356/2076-6734-2016-2-221-234
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre albedo
Arctic
Arctic Basin
Arctic
Arctic Ocean
Global warming
Sea ice
genre_facet albedo
Arctic
Arctic Basin
Arctic
Arctic Ocean
Global warming
Sea ice
op_source Ice and Snow; Том 56, № 2 (2016); 221-234
Лёд и Снег; Том 56, № 2 (2016); 221-234
2412-3765
2076-6734
10.15356/2076-6734-2016-2
op_relation https://ice-snow.igras.ru/jour/article/view/301/168
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spelling ftjias:oai:oai.ice.elpub.ru:article/301 2023-05-15T13:11:45+02:00 History of sea ice in the Arctic basin: Lessons from the past for future История оледенения Арктического бассейна: взгляд из прошлого для оценки возможных изменений в будущем I. Borzenkova I. И. Борзенкова И. 2016-05-10 application/pdf https://ice-snow.igras.ru/jour/article/view/301 https://doi.org/10.15356/2076-6734-2016-2-221-234 rus rus IGRAS https://ice-snow.igras.ru/jour/article/view/301/168 Алексеев Г.В. Арктическое измерение глобального потепления // Лёд и Снег. 2014. № 2 (126). С. 53–68. Алексеев Г.В., Булатов Л.В., Захаров В.Ф., Иванов В.Ц. Поступление необычайно теплых атлантических вод в Арктический бассейн // ДАН. 1997. Т. 356. № 3. С. 401–403. Анисимов О.А., Жирков А.Ф., Шерстюков А.Б. Современные изменения криосферы и природной среды в Арктике // Арктика. XXI век. Естественные науки. 2015. Т. 2. № 3. С. 24–47. Борзенкова И.И. 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CC-BY Ice and Snow; Том 56, № 2 (2016); 221-234 Лёд и Снег; Том 56, № 2 (2016); 221-234 2412-3765 2076-6734 10.15356/2076-6734-2016-2 Arctic current global warming history of sea icing last 65 million years sea ice the Cenozoic time история образования морских льдов;кайнозой;морские льды;последние 65 млн лет;современное глобальное потепление info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2016 ftjias https://doi.org/10.15356/2076-6734-2016-2-221-234 https://doi.org/10.15356/2076-6734-2016-2 https://doi.org/10.15356/2076-6734-2015-2-81-92 https://doi.org/10.15356/2076-6734-2015-3-73-82 https://doi.org/10.1029/2007PA001479 https://doi.org/10.1 2022-12-20T13:29:44Z The process of the sea ice formation in the Arctic Ocean is analyzed for the period of the last 65 million years, i.e. from the Paleocene to the present time. Appearance of sea ice in the high latitudes is demonstrated to be caused by the negative trend in global temperatures due to decreasing of the CO2 concentration in the ancient atmosphere. Formation of seasonal and perennial ice cover in the limited area near the Pole could take place during the mid-Neogene period, about 12–13 Ma ago. However, areas of the sea icing could be obviously changed for this time during periods of the climate warming and cooling. Permanent sea ice had been formed in the early Pleistocene, i.e. about 2.0–1.8 Ma ago only. Paleoclimatic reconstructions, based on the indirect data and modeling simulation for the Holocene optimum (10–6 ka ago) and for the Last Interglacial period (the isotopic substage in the marine cross-section 5e, about 125–127 ka ago) had shown that rising of global temperatures by 1.0–1.5 °C resulted in strong decreasing of the sea ice area, and the perennial ice cover became the seasonal one. Relatively small changes in the incoming solar radiation originating during the spring-summer time due to the orbital factors played the role of a trigger for onset of the melting process. Further on, the process could be enhanced owing to difference in the albedo between the ice cover and open water. Recently, the rapid shortening of the sea ice area is noted, and in some parts of the Arctic Ocean the area is twice cut down as compared with the normal. In 2015, the record low area of the winter sea ice was observed, and therewith the maximum of the ice area shifted to the earlier period (by 15 days) as compared with the period of 1981–2010. The winter fluctuations of the sea ice areas are as much important as the summer ones, since they are the best indicators of the present-day global warming. Thus, it can be supposed that some mechanism of replacing the perennial sea ice by the seasonal ones has been started up, that is ... Article in Journal/Newspaper albedo Arctic Arctic Basin Arctic Arctic Ocean Global warming Sea ice Ice and Snow (E-Journal) Arctic Arctic Ocean Ice and Snow 56 2 221 234

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