Arctic dimension of global warming

A brief assessment of the global warming in the Arctic climate system with the emphasis on sea ice is presented. The Arctic region is coupled to the global climate system by the atmosphere and ocean circulation that providesa major contribution to the Arctic energy budget. On this basis using of spe...

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Published in:Ice and Snow
Main Authors: G. Alekseev V., Г. Алексеев В.
Format: Article in Journal/Newspaper
Language:Russian
Published: IGRAS 2015
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/41
https://doi.org/10.15356/2076-6734-2014-2-53-68
id ftjias:oai:oai.ice.elpub.ru:article/41
record_format openpolar
institution Open Polar
collection Ice and Snow (E-Journal)
op_collection_id ftjias
language Russian
topic Arctic;Arctic and global warming;climate change;heat transport
Арктика;арктическое и глобальное потепление;изменения климата;перенос тепла
spellingShingle Arctic;Arctic and global warming;climate change;heat transport
Арктика;арктическое и глобальное потепление;изменения климата;перенос тепла
G. Alekseev V.
Г. Алексеев В.
Arctic dimension of global warming
topic_facet Arctic;Arctic and global warming;climate change;heat transport
Арктика;арктическое и глобальное потепление;изменения климата;перенос тепла
description A brief assessment of the global warming in the Arctic climate system with the emphasis on sea ice is presented. The Arctic region is coupled to the global climate system by the atmosphere and ocean circulation that providesa major contribution to the Arctic energy budget. On this basis using of special indices it is shown that amplification of warming in the Arctic is associated with the increasing of meridional heat transport from the low latitudes. Дан обзор проявлений глобального потепления в арктической климатической системе. Особое внимание уделено морскому ледяному покрову. Арктика объединена с глобальной климатической системой циркуляцией атмосферы и океана, вносящей основной вклад в формирование энергетического баланса. Исходя из этого, с помощью специальных индексов показано, что усиление потепления в Арктике связано c ростом меридионального переноса тепла из низких широт, а зональная составляющая атмосферного переноса влияет на потепление в умеренных широтах. Кроме того, установлено, что часть современного глобального потепления также связана с ростом переноса тепла. В арктическое усиление потепления вносит вклад и увеличение приходящей к поверхности длинноволновой радиации за счёт повышения влажности и облачности в арктической атмосфере. Возрастающее отступление кромки льда в конце летнего сезона от берегов Сибири и Аляски в результате повышения летней температуры воздуха способствует прогреву верхнего слоя морской воды и усилению потепления в октябре–январе. Дана схема арктического усиления потепления в результате роста меридионального переноса из низких широт и возникающих обратных связей в арктической климатической системе.
format Article in Journal/Newspaper
author G. Alekseev V.
Г. Алексеев В.
author_facet G. Alekseev V.
Г. Алексеев В.
author_sort G. Alekseev V.
title Arctic dimension of global warming
title_short Arctic dimension of global warming
title_full Arctic dimension of global warming
title_fullStr Arctic dimension of global warming
title_full_unstemmed Arctic dimension of global warming
title_sort arctic dimension of global warming
publisher IGRAS
publishDate 2015
url https://ice-snow.igras.ru/jour/article/view/41
https://doi.org/10.15356/2076-6734-2014-2-53-68
geographic Arctic
geographic_facet Arctic
genre Arctic
Arctic
Climate change
Global warming
Sea ice
Арктика
genre_facet Arctic
Arctic
Climate change
Global warming
Sea ice
Арктика
op_source Ice and Snow; Том 54, № 2 (2014); 53-68
Лёд и Снег; Том 54, № 2 (2014); 53-68
2412-3765
2076-6734
10.15356/2076-6734-2014-2
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spelling ftjias:oai:oai.ice.elpub.ru:article/41 2023-05-15T14:26:51+02:00 Arctic dimension of global warming Арктическое измерение глобального потепления G. Alekseev V. Г. Алексеев В. 2015-03-26 https://ice-snow.igras.ru/jour/article/view/41 https://doi.org/10.15356/2076-6734-2014-2-53-68 ru rus IGRAS Alekseev G.V. Interrelation between ocean and atmosphere as thermodynamic process. Trudy AANII. Proc. of AARI. 1982, 383: 25–34. [In Russian]. Alekseev G.V. Studies of Arctic climate change in XX century. Trudy AANII. Proc. of AARI. 2003, 446: 6–21. [In Russian]. Alekseev G.V. Role of the atmospheric circulation and other factors in the formation of Arctic climate. Formirovanie i dinamika sovremennogo klimata Arktiki. Formation and dynamics of the present-day Arctic climate. Ed. G.V. Alexeev. Sankt-Petersburg: Hydrometeoizdat: 2004: 27–46. [In Russian]. Alekseev G.V., Podgornyi I.A., Svyashchennikov P.N. Advective and radiation changes of climate. Doklady Akademii Nauk. Proc. of the Academy of Sciences. 1990, 315 (4): 824–827. [In Russian]. Alekseev G.V., Podgornyi I.A. Role of advection and other factors in the polar climate formation. Klimaticheskiy rezhim Arktiki na rubezhe XX i XXI vv. Climatic regime of Arctic on the boundary of XX and XXI centuries. Ed. B.A. Krutskikh. Sankt-Petersburg: Hydrometeoizdat, 1991: 4–18. [In Russian]. Alekseev G.V., Podgornyi I.A., Svyashchennikov P.N. Changes of the warming influence of oceans to the global climate. Doklady Akademii Nauk. Proc. of the Academy of Sciences. 1991, 320 № (1): 70–73. [In Russian]. Alekseev G.V., Svyashchennikov P.N. Estestvennaya izmenchivost’ kharakteristik klimata Severnoy polyarnoy oblasti b Severnogo polushariya. Natural changeability of climate characteristics of the North Polar Region and Northern Hemisphere. Leningrad: Hydrometeoizdat, 1991: 159 p. [In Russian]. Alekseev G.V., Nagurnyi A.P. Role of sea ice in the formation of annual cycle of the carbon dioxide in Arctic. Doklady Akademii Nauk. Proc. of the Academy of Sciences. 2007, 417 (4): 541–544. [In Russian]. Alekseev G.V., Nagurnyi A.P., Makshtas A.P., Ivanov N.E., Shutilin S.V. Role of sea ice in the formation of annual cycle of the carbon dioxide in high latitude marine Arctic. Problemy Arktiki i Antarktiki. Problems of Arctic and Antarctic. 2007, 77: 28–36. [In Russian]. Alekseev G.V., Danilov A.I., Kattsov V.M., Kuz’mina S.I., Ivanov N.E. Sea ice in the Northern Hemisphere in connection with climate change in XX and XXI centuries according to the data of observation and modeling. Izvestiya Ross. Akad. Nauk. Fizika atmosfery i okeana. Proc. of RAS. Physics of Atmosphere and Ocean. 2009, 45 (6): 723–735. [In Russian]. Alexeev G.V., Ivanov N.E., Pnyushkov A.B., Kharlanenkova N.E. Climate changes in the marine Arctic during beginning of XXI century. Meteorologicheskie i geofizicyeskie issledovaniya. Meteorology and Geophysics Studies. Moscow, 2011: 3–25. [In Russian]. Blinova E.N. Hydrodynamic theory of pressure waves and centers of atmosphere action Doklady Akademii Nauk. Proc. of the Academy of Sciences. 1943, 39: 284–287. [In Russian]. Budyko M.I. Climate change. Leningrad: Hydrometeoizdat, 1974: 280 p. [In Russian]. Van Migem J. Energetic of the atmosphere. Ed. L.T. Matveeva. Leningrad: Hydrometeoizdat, 1977: 327 p. [In Russian]. Vangengeim G.Ya. On the oscillations of atmospheric circulation above the Northern Hemisphere. Izvestiya Ross. Akad. Nauk. Ser. geofizicheskaya i geiograficheskaya. Izvestiya of the Russian Academy of Sciences. Ser. Geophysics and Geography. 1946, 10 (5): 405–416. [In Russian]. Vasyuta Yu.V., Mokhov I.I., Petukhov V.K. Sensitivity of the little parametric climate models to the changes of characteristics of the meridional heat transfer. Izvestiya Ross. Akad. Nauk. Fizika atmosfery i okeana. Proc. of the USSR Academy of Sciences. Physics of Atmosphere and Ocean. 1988, 24 (2): 115–125. [In Russian]. Vize V.Yu. 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CC-BY Ice and Snow; Том 54, № 2 (2014); 53-68 Лёд и Снег; Том 54, № 2 (2014); 53-68 2412-3765 2076-6734 10.15356/2076-6734-2014-2 Arctic;Arctic and global warming;climate change;heat transport Арктика;арктическое и глобальное потепление;изменения климата;перенос тепла info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftjias https://doi.org/10.15356/2076-6734-2014-2-53-68 https://doi.org/10.15356/2076-6734-2014-2 https://doi.org/10.1029/2003JC002120 https://doi.org/10.1029/2005GL024481 https://doi.org/10.1029/134GM01 https://doi.org/10.1175/JCLI-D-11-00449.1 https 2022-12-20T13:30:18Z A brief assessment of the global warming in the Arctic climate system with the emphasis on sea ice is presented. The Arctic region is coupled to the global climate system by the atmosphere and ocean circulation that providesa major contribution to the Arctic energy budget. On this basis using of special indices it is shown that amplification of warming in the Arctic is associated with the increasing of meridional heat transport from the low latitudes. Дан обзор проявлений глобального потепления в арктической климатической системе. Особое внимание уделено морскому ледяному покрову. Арктика объединена с глобальной климатической системой циркуляцией атмосферы и океана, вносящей основной вклад в формирование энергетического баланса. Исходя из этого, с помощью специальных индексов показано, что усиление потепления в Арктике связано c ростом меридионального переноса тепла из низких широт, а зональная составляющая атмосферного переноса влияет на потепление в умеренных широтах. Кроме того, установлено, что часть современного глобального потепления также связана с ростом переноса тепла. В арктическое усиление потепления вносит вклад и увеличение приходящей к поверхности длинноволновой радиации за счёт повышения влажности и облачности в арктической атмосфере. Возрастающее отступление кромки льда в конце летнего сезона от берегов Сибири и Аляски в результате повышения летней температуры воздуха способствует прогреву верхнего слоя морской воды и усилению потепления в октябре–январе. Дана схема арктического усиления потепления в результате роста меридионального переноса из низких широт и возникающих обратных связей в арктической климатической системе. Article in Journal/Newspaper Arctic Arctic Climate change Global warming Sea ice Арктика Ice and Snow (E-Journal) Arctic Ice and Snow 126 2 53