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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Norwegian Polar Institute
2016
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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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1766307597798866944 |