Lagrangian analysis of sea-ice dynamics in the Arctic Ocean

In this study, we present Lagrangian diagnostics to quantify changes in the dynamical characteristics of the Arctic sea-ice cover from 2006 to 2014. Examined in particular is the evolution in finite-time Lyapunov exponents (FTLEs), which monitor the rate at which neighbouring particle trajectories d...

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Bibliographic Details
Published in:Polar Research
Main Authors: Sándor Szanyi, Jennifer V. Lukovich, David G. Barber
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2016
Subjects:
LAD
Online Access:https://doi.org/10.3402/polar.v35.30778
https://doaj.org/article/7a817140550b4a9b8f3ca4205e0bebb4
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spelling ftdoajarticles:oai:doaj.org/article:7a817140550b4a9b8f3ca4205e0bebb4 2023-05-15T14:34:35+02:00 Lagrangian analysis of sea-ice dynamics in the Arctic Ocean Sándor Szanyi Jennifer V. Lukovich David G. Barber 2016-11-01T00:00:00Z https://doi.org/10.3402/polar.v35.30778 https://doaj.org/article/7a817140550b4a9b8f3ca4205e0bebb4 EN eng Norwegian Polar Institute http://www.polarresearch.net/index.php/polar/article/view/30778/50215 https://doaj.org/toc/1751-8369 1751-8369 doi:10.3402/polar.v35.30778 https://doaj.org/article/7a817140550b4a9b8f3ca4205e0bebb4 Polar Research, Vol 35, Iss 0, Pp 1-9 (2016) sea-ice dynamics FTLE Arctic Ocean Lagrangian diagnostics LAD Environmental sciences GE1-350 Oceanography GC1-1581 article 2016 ftdoajarticles https://doi.org/10.3402/polar.v35.30778 2022-12-31T11:49:11Z In this study, we present Lagrangian diagnostics to quantify changes in the dynamical characteristics of the Arctic sea-ice cover from 2006 to 2014. Examined in particular is the evolution in finite-time Lyapunov exponents (FTLEs), which monitor the rate at which neighbouring particle trajectories diverge, and stretching rates throughout the Arctic. In this analysis, we compute FTLEs for the Arctic ice-drift field using the 62.5 km daily sea-ice motion vector data from the European Organisation for the Exploitation of Meteorological Satellites Ocean and Sea Ice Satellite Application Facility. Results from the FTLE analysis highlight the existence of three distinct dynamical regions with strong stretching, captured by FTLE maxima or ridges. It is further shown that FTLE ridges are dominated by shear, with contributions from divergence in the Beaufort Sea. Localization of FTLE features following the 2012 record minimum in summertime sea-ice extent illustrates the emergence of an Arctic characterized by increased mixing. Results also demonstrate higher FTLEs in years when lower multi-year ice extent is observed. Article in Journal/Newspaper Arctic Arctic Ocean Beaufort Sea Polar Research Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Polar Research 35 1 30778
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic sea-ice dynamics
FTLE
Arctic Ocean
Lagrangian diagnostics
LAD
Environmental sciences
GE1-350
Oceanography
GC1-1581
spellingShingle sea-ice dynamics
FTLE
Arctic Ocean
Lagrangian diagnostics
LAD
Environmental sciences
GE1-350
Oceanography
GC1-1581
Sándor Szanyi
Jennifer V. Lukovich
David G. Barber
Lagrangian analysis of sea-ice dynamics in the Arctic Ocean
topic_facet sea-ice dynamics
FTLE
Arctic Ocean
Lagrangian diagnostics
LAD
Environmental sciences
GE1-350
Oceanography
GC1-1581
description In this study, we present Lagrangian diagnostics to quantify changes in the dynamical characteristics of the Arctic sea-ice cover from 2006 to 2014. Examined in particular is the evolution in finite-time Lyapunov exponents (FTLEs), which monitor the rate at which neighbouring particle trajectories diverge, and stretching rates throughout the Arctic. In this analysis, we compute FTLEs for the Arctic ice-drift field using the 62.5 km daily sea-ice motion vector data from the European Organisation for the Exploitation of Meteorological Satellites Ocean and Sea Ice Satellite Application Facility. Results from the FTLE analysis highlight the existence of three distinct dynamical regions with strong stretching, captured by FTLE maxima or ridges. It is further shown that FTLE ridges are dominated by shear, with contributions from divergence in the Beaufort Sea. Localization of FTLE features following the 2012 record minimum in summertime sea-ice extent illustrates the emergence of an Arctic characterized by increased mixing. Results also demonstrate higher FTLEs in years when lower multi-year ice extent is observed.
format Article in Journal/Newspaper
author Sándor Szanyi
Jennifer V. Lukovich
David G. Barber
author_facet Sándor Szanyi
Jennifer V. Lukovich
David G. Barber
author_sort Sándor Szanyi
title Lagrangian analysis of sea-ice dynamics in the Arctic Ocean
title_short Lagrangian analysis of sea-ice dynamics in the Arctic Ocean
title_full Lagrangian analysis of sea-ice dynamics in the Arctic Ocean
title_fullStr Lagrangian analysis of sea-ice dynamics in the Arctic Ocean
title_full_unstemmed Lagrangian analysis of sea-ice dynamics in the Arctic Ocean
title_sort lagrangian analysis of sea-ice dynamics in the arctic ocean
publisher Norwegian Polar Institute
publishDate 2016
url https://doi.org/10.3402/polar.v35.30778
https://doaj.org/article/7a817140550b4a9b8f3ca4205e0bebb4
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Beaufort Sea
Polar Research
Sea ice
genre_facet Arctic
Arctic Ocean
Beaufort Sea
Polar Research
Sea ice
op_source Polar Research, Vol 35, Iss 0, Pp 1-9 (2016)
op_relation http://www.polarresearch.net/index.php/polar/article/view/30778/50215
https://doaj.org/toc/1751-8369
1751-8369
doi:10.3402/polar.v35.30778
https://doaj.org/article/7a817140550b4a9b8f3ca4205e0bebb4
op_doi https://doi.org/10.3402/polar.v35.30778
container_title Polar Research
container_volume 35
container_issue 1
container_start_page 30778
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