CLIMATIC IMPLICATIONS OF THE FRESH WATER EXPANSION IN THE GREENLAND SEA AND THE NORTH ATLANTIC

In second part of XX century there are three valuable salinity anomalies in North Atlantic, so-called «The Great Salinity Anomaly» (GSA), which can be characterized as a large, near-surface pool of fresher water [31–33, 36, 37]. There are GSA’70s, GSA’80s and GSA’90s. Dickson [37] described this eve...

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Published in:Marine Chemistry
Main Authors: A. Popov V., A. Rubchenya V., А. Попов В., А. Рубченя В.
Format: Article in Journal/Newspaper
Language:Russian
Published: IGRAS 2015
Subjects:
Атлантика
Гренландское море
климат
ледовитость
полынья
Северный Ледовитый океан
соленосная аномалия
тренды
Arctic
Climate change
Greenland
Greenland Sea
North Atlantic
Online Access:https://ice-snow.igras.ru/jour/article/view/230
https://doi.org/10.15356/2076-6734-2012-2-81-96
id ftjias:oai:oai.ice.elpub.ru:article/230
record_format openpolar
institution Open Polar
collection Ice and Snow
op_collection_id ftjias
language Russian
topic Атлантика
Гренландское море
климат
ледовитость
полынья
Северный Ледовитый океан
соленосная аномалия
тренды
spellingShingle Атлантика
Гренландское море
климат
ледовитость
полынья
Северный Ледовитый океан
соленосная аномалия
тренды
A. Popov V.
A. Rubchenya V.
А. Попов В.
А. Рубченя В.
CLIMATIC IMPLICATIONS OF THE FRESH WATER EXPANSION IN THE GREENLAND SEA AND THE NORTH ATLANTIC
topic_facet Атлантика
Гренландское море
климат
ледовитость
полынья
Северный Ледовитый океан
соленосная аномалия
тренды
description In second part of XX century there are three valuable salinity anomalies in North Atlantic, so-called «The Great Salinity Anomaly» (GSA), which can be characterized as a large, near-surface pool of fresher water [31–33, 36, 37]. There are GSA’70s, GSA’80s and GSA’90s. Dickson [37] described this event as one of dramatic and prolonged changes in ocean’s climate in XX century. In this paper, we have shown genesis of GSA’70s connected with ice production in Arctic flaw leads. Formation of GSAs’ in 1980s and 1990s has, at least, two main reasons. First is fresh water pools and huge amounts of ice carried out fromArcticBasin. The second one is recirculation of previous salinity anomaly inSubarcticBasin. Phenomenological model of climate change formation in polar and subpolar zone of North Hemisphere is presented in the paper. Examination conditions of previous GSA’s appearance and analysis of valuable fresh water intrusions in North Atlantic allow us to conclude that conditions for GSA’2010s are formed already and started to propagate inNorth Atlantic. For the first time we described GSA during its appearance, not post factum. Thus, we are standing at the break point of relatively long cooling inArctic. Во второй половине ХХ в. в Северной Атлантике отмечено три значимых аномалии распреснения поверхностных вод. В иностранной литературе они получили собственное имя – Великая соленосная аномалия (ВСА) [31–33, 36, 37]. Выделяют ВСА-1970-х, ВСА-1980-х и ВСА-1990-х годов. Р. Диксон [37] описал это явление как одно из наиболее резко и продолжительно влияющих на изменения климата океана в ХХ в. По мнению авторов настоящей статьи, генезис ВСА-1970-х связан с ледопродуктивностью арктических заприпайных полыней. В этой статье даётся феноменологическая модель формирования климатических изменений в зоне полярных и умеренных широт Северного полушария, обусловленных периодическими выбросами в Северную Атлантику аномально больших объёмов распреснённых вод из Северного Ледовитого океана. Делается вывод, что в настоящий момент уже ...
format Article in Journal/Newspaper
author A. Popov V.
A. Rubchenya V.
А. Попов В.
А. Рубченя В.
author_facet A. Popov V.
A. Rubchenya V.
А. Попов В.
А. Рубченя В.
author_sort A. Popov V.
title CLIMATIC IMPLICATIONS OF THE FRESH WATER EXPANSION IN THE GREENLAND SEA AND THE NORTH ATLANTIC
title_short CLIMATIC IMPLICATIONS OF THE FRESH WATER EXPANSION IN THE GREENLAND SEA AND THE NORTH ATLANTIC
title_full CLIMATIC IMPLICATIONS OF THE FRESH WATER EXPANSION IN THE GREENLAND SEA AND THE NORTH ATLANTIC
title_fullStr CLIMATIC IMPLICATIONS OF THE FRESH WATER EXPANSION IN THE GREENLAND SEA AND THE NORTH ATLANTIC
title_full_unstemmed CLIMATIC IMPLICATIONS OF THE FRESH WATER EXPANSION IN THE GREENLAND SEA AND THE NORTH ATLANTIC
title_sort climatic implications of the fresh water expansion in the greenland sea and the north atlantic
publisher IGRAS
publishDate 2015
url https://ice-snow.igras.ru/jour/article/view/230
https://doi.org/10.15356/2076-6734-2012-2-81-96
genre Arctic
Climate change
Greenland
Greenland Sea
North Atlantic
Гренландское море
genre_facet Arctic
Climate change
Greenland
Greenland Sea
North Atlantic
Гренландское море
op_source Ice and Snow; Том 52, № 2 (2012); 81-96
Лёд и Снег; Том 52, № 2 (2012); 81-96
2412-3765
2076-6734
10.15356/2076-6734-2012-2
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spelling ftjias:oai:oai.ice.elpub.ru:article/230 2024-09-15T17:50:54+00:00 CLIMATIC IMPLICATIONS OF THE FRESH WATER EXPANSION IN THE GREENLAND SEA AND THE NORTH ATLANTIC КЛИМАТИЧЕСКИЕ ПОСЛЕДСТВИЯ ЭКСПАНСИИ ПРЕСНЫХ ВОД В ГРЕНЛАНДСКОЕ МОРЕ И СЕВЕРНУЮ АТЛАНТИКУ A. Popov V. A. Rubchenya V. А. Попов В. А. Рубченя В. 2015-11-15 https://ice-snow.igras.ru/jour/article/view/230 https://doi.org/10.15356/2076-6734-2012-2-81-96 ru rus IGRAS Alekseev G.V. Naturnye issledovaniya krupnomasshtabnoy izmenchivosti v okeane. Natural studies of large-scale changeability in the ocean. Leningrad: Hydrometeoizdat, 1984: 111 p. [In Russian]. Alekseev G.V., Svyashchennikov P.N. Estestvennaya izmenchivost’ kharakteristik klimata Severnoy polyarnoy oblasti i Severnogo polushariya. Natural changeability of the climate characteristics in North Polar Region and in the Northern Hemisphere. Leningrad: Hydrometeoizdat, 1991: 159 p. [In Russian]. Alekseev G.V., Ivanov N.E., Pnyushkov A.V., Balakin A.A. Changes of climate in the maritime Arctic in the beginning of 21st century. Problemy Arktiki i Antarktiki. Problems of Arctic and Antarctic. 2010, 3 (86): 22–34. [In Russian]. Volkov N.A., Gudkovich Z.M. Main results of the ice drift study in the Arctic basin. Problemy Arktiki i Antarktiki. Problems of Arctic and Antarctic. 1967, 27: 55–64. [In Russian]. Girs A.A. Role of atmospheric circulation in the formation of heat regime in Arctic. Problemy Arktiki i Antarktiki. Problems of Arctic and Antarctic. 1967, 25: 5–22. [In Russian]. Girs A.A. Taking into account the development of macrosynoptic processes under study of causes the changes of background characteristics of hydrosphere. Issledovaniya po probleme okean – atmosfera. Studies of problem “ocean – atmosphere”. Trudy LGMI. Proc. of Leningrad Hydromet. Institute. Issue 32. Leningrad: Gidrometeoizdat. Leningrad: Hydrometeoizdat, 1970: 145–168. [In Russian]. Girs A.A. Mnogoletnie kolebaniya atmosfernoy tsirkulyatsii i dolgosrochnye gidrometeorologicheskie prognozy. Long-term changes of atmospheric circulation and long-term hydrometeorological predictions. Leningrad: Hydrometeoizdat, 1971: 280 p. [In Russian]. Gudkovich Z.M., Kovalev E.G. Fluctuations of ice coverage in Russian Arctic seas in 20th century and assessment of its possible changes in 21st century. Materialy nauchno-prakticheskogo soveshchaniya. Materials of scientific meeting. St.-Petersburg: AARI, 2002: 36–45. [In Russian]. Gudkovich Z.M., Kovalev E.G. On some mechanisms of cyclic climate changes in Arctic and Antarctic. Okeanologiya. Oceanology. 2002, 42 (6): 815–821. [In Russian]. Gudkovich Z.M., Karklbn V.P., Frolov I.E. Intrasecular climate variations, areas of ice cover in Eurasian Arctic seas and their possible reasons. Meteorologiya i gidrologiya. Meteorology and Hydrology. 2005, 6: 5–13. [In Russian]. Ezhegodhyi informatsionnyi byulleten’. 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Ice and Snow; Том 52, № 2 (2012); 81-96 Лёд и Снег; Том 52, № 2 (2012); 81-96 2412-3765 2076-6734 10.15356/2076-6734-2012-2 Атлантика Гренландское море климат ледовитость полынья Северный Ледовитый океан соленосная аномалия тренды info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftjias https://doi.org/10.15356/2076-6734-2012-2-81-9610.15356/2076-6734-2012-210.1029/2003GL019334 2024-06-28T03:05:47Z In second part of XX century there are three valuable salinity anomalies in North Atlantic, so-called «The Great Salinity Anomaly» (GSA), which can be characterized as a large, near-surface pool of fresher water [31–33, 36, 37]. There are GSA’70s, GSA’80s and GSA’90s. Dickson [37] described this event as one of dramatic and prolonged changes in ocean’s climate in XX century. In this paper, we have shown genesis of GSA’70s connected with ice production in Arctic flaw leads. Formation of GSAs’ in 1980s and 1990s has, at least, two main reasons. First is fresh water pools and huge amounts of ice carried out fromArcticBasin. The second one is recirculation of previous salinity anomaly inSubarcticBasin. Phenomenological model of climate change formation in polar and subpolar zone of North Hemisphere is presented in the paper. Examination conditions of previous GSA’s appearance and analysis of valuable fresh water intrusions in North Atlantic allow us to conclude that conditions for GSA’2010s are formed already and started to propagate inNorth Atlantic. For the first time we described GSA during its appearance, not post factum. Thus, we are standing at the break point of relatively long cooling inArctic. Во второй половине ХХ в. в Северной Атлантике отмечено три значимых аномалии распреснения поверхностных вод. В иностранной литературе они получили собственное имя – Великая соленосная аномалия (ВСА) [31–33, 36, 37]. Выделяют ВСА-1970-х, ВСА-1980-х и ВСА-1990-х годов. Р. Диксон [37] описал это явление как одно из наиболее резко и продолжительно влияющих на изменения климата океана в ХХ в. По мнению авторов настоящей статьи, генезис ВСА-1970-х связан с ледопродуктивностью арктических заприпайных полыней. В этой статье даётся феноменологическая модель формирования климатических изменений в зоне полярных и умеренных широт Северного полушария, обусловленных периодическими выбросами в Северную Атлантику аномально больших объёмов распреснённых вод из Северного Ледовитого океана. Делается вывод, что в настоящий момент уже ... Article in Journal/Newspaper Arctic Climate change Greenland Greenland Sea North Atlantic Гренландское море Ice and Snow Marine Chemistry 197 11 25

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