Articles | Volume 17, issue 4
https://doi.org/10.5194/tc-17-1545-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-17-1545-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
11 Apr 2023
Research article |
| 11 Apr 2023
| 11 Apr 2023
A quasi-objective single-buoy approach for understanding Lagrangian coherent structures and sea ice dynamics
Nikolas O. Aksamit
CORRESPONDING AUTHOR
Department of Geography, University of Victoria, Victoria, BC V8P 5C2, Canada
School of Earth and Environment, University of Canterbury, Christchurch 8041, New Zealand
now at: Department of Mathematics and Statistics, UiT – The Arctic University of Norway, Tromsø, Norway
Randall K. Scharien
Department of Geography, University of Victoria, Victoria, BC V8P 5C2, Canada
Jennifer K. Hutchings
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
Jennifer V. Lukovich
Centre for Earth Observation Science, University of Manitoba, Winnipeg, MB R3T 2N2, Canada
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Short summary
Coherent flow patterns in sea ice have a significant influence on sea ice fracture and refreezing. We can better understand the state of sea ice, and its influence on the atmosphere and ocean, if we understand these structures. By adapting recent developments in chaotic dynamical systems, we are able to approximate ice stretching surrounding individual ice buoys. This illuminates the state of sea ice at much higher resolution and allows us to see previously invisible ice deformation patterns.
Coherent flow patterns in sea ice have a significant influence on sea ice fracture and...
