Dramatic decline of Arctic sea ice linked to global warming

Abstract Arctic sea ice has declined rapidly over the past four decades at the rate of − 4.7% per decade leading to an imbalance in the oceanic heat flux. The study reported that the July 2019 was the warmest month in the Arctic, leading to a substantial sea ice loss in the last 41 years. Consequent...

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Main Authors: Juhi Yadav, Avinash Kumar, Rahul Mohan
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:http://link.springer.com/10.1007/s11069-020-04064-y
id ftrepec:oai:RePEc:spr:nathaz:v::y::i::d:10.1007_s11069-020-04064-y
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spelling ftrepec:oai:RePEc:spr:nathaz:v::y::i::d:10.1007_s11069-020-04064-y 2023-05-15T14:49:33+02:00 Dramatic decline of Arctic sea ice linked to global warming Juhi Yadav Avinash Kumar Rahul Mohan http://link.springer.com/10.1007/s11069-020-04064-y unknown http://link.springer.com/10.1007/s11069-020-04064-y article ftrepec 2020-12-04T13:40:57Z Abstract Arctic sea ice has declined rapidly over the past four decades at the rate of − 4.7% per decade leading to an imbalance in the oceanic heat flux. The study reported that the July 2019 was the warmest month in the Arctic, leading to a substantial sea ice loss in the last 41 years. Consequently, during this month, the lowest sea ice extent (SIE, 7.5 million km2) and sea ice volume (8900 km3) were recorded. The decadal trend of sea ice decline in September 2019 has reached to ca. − 13% per decade. The latest record shows that average SIE during summer 2019 (5.65 million km2) has set a new lowest record after 2012 (5.32 million km2), since the sea ice formation process has been largely hampered during the summer months. The study reveals that the land–ocean warming processes intensifying the sea ice loss and also leading in disruption of the global ocean circulation. Sea ice extent, Ocean–atmosphere, Global warming, Satellite remote sensing, Northern hemisphere Article in Journal/Newspaper Arctic Global warming Sea ice RePEc (Research Papers in Economics) Arctic
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Abstract Arctic sea ice has declined rapidly over the past four decades at the rate of − 4.7% per decade leading to an imbalance in the oceanic heat flux. The study reported that the July 2019 was the warmest month in the Arctic, leading to a substantial sea ice loss in the last 41 years. Consequently, during this month, the lowest sea ice extent (SIE, 7.5 million km2) and sea ice volume (8900 km3) were recorded. The decadal trend of sea ice decline in September 2019 has reached to ca. − 13% per decade. The latest record shows that average SIE during summer 2019 (5.65 million km2) has set a new lowest record after 2012 (5.32 million km2), since the sea ice formation process has been largely hampered during the summer months. The study reveals that the land–ocean warming processes intensifying the sea ice loss and also leading in disruption of the global ocean circulation. Sea ice extent, Ocean–atmosphere, Global warming, Satellite remote sensing, Northern hemisphere
format Article in Journal/Newspaper
author Juhi Yadav
Avinash Kumar
Rahul Mohan
spellingShingle Juhi Yadav
Avinash Kumar
Rahul Mohan
Dramatic decline of Arctic sea ice linked to global warming
author_facet Juhi Yadav
Avinash Kumar
Rahul Mohan
author_sort Juhi Yadav
title Dramatic decline of Arctic sea ice linked to global warming
title_short Dramatic decline of Arctic sea ice linked to global warming
title_full Dramatic decline of Arctic sea ice linked to global warming
title_fullStr Dramatic decline of Arctic sea ice linked to global warming
title_full_unstemmed Dramatic decline of Arctic sea ice linked to global warming
title_sort dramatic decline of arctic sea ice linked to global warming
url http://link.springer.com/10.1007/s11069-020-04064-y
geographic Arctic
geographic_facet Arctic
genre Arctic
Global warming
Sea ice
genre_facet Arctic
Global warming
Sea ice
op_relation http://link.springer.com/10.1007/s11069-020-04064-y
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