Articles | Volume 19, issue 8
https://doi.org/10.5194/tc-19-3065-2025
https://doi.org/10.5194/tc-19-3065-2025
Research article
 | 
15 Aug 2025
Research article |  | 15 Aug 2025

Estimation of duration and its changes in Lagrangian observations relying on ice floes in the Arctic Ocean utilizing a sea ice motion product

Fanyi Zhang, Ruibo Lei, Meng Qu, Na Li, Ying Chen, and Xiaoping Pang

Data sets

Polar Pathfinder Daily 25 km EASE-Grid Sea Ice Motion Vectors M. Tschudi et al. https://doi.org/10.5067/INAWUWO7QH7B

NOAA/NSIDC Climate Data Record of Passive Microwave Sea Ice Concentration W. N. Meier et al. https://doi.org/10.7265/efmz-2t65

ERA5 hourly data on single levels from 1940 to present H. Hersbach et al. https://doi.org/10.24381/cds.adbb2d47

A weekly Arctic sea-ice thickness data record from merged CryoSat-2 and SMOS satellite data (https://data.seaiceportal.de/data/cs2smos_awi/v204/) R. Ricker et al. https://doi.org/10.5194/tc-11-1607-2017

Maritime Boundaries Geodatabase: Maritime Boundaries and Exclusive Economic Zones (200NM) Flanders Marine Institute https://doi.org/10.14284/632

Snow height and air temperature on sea ice from Snow Buoy measurements M. Nicolaus et al. https://doi.org/10.1594/PANGAEA.875638

International Arctic Buoy Programme, digital media International Arctic Buoy Programme https://iabp.apl.uw.edu/TABLES/ArcticTable.html

DAMOCLES 2007-2008 - Hamburg Arctic Ocean Buoy Drift Experiment: meteorological measurements of 16 autonomous drifting ice buoys B. Brümmer et al. https://doi.org/10.1594/WDCC/UNI_HH_MI_DAMOCLES2007

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Short summary
We reconstructed sea ice drift trajectories and identified optimal deployment areas for Lagrangian observations in the central Arctic Ocean. The trajectories revealed a preference for ice advection towards the Transpolar Drift region over the Beaufort Gyre, with endpoints influenced by large-scale atmospheric circulation patterns. This study provides critical support for the planning and implementation of Lagrangian observations relying on ice floes in the central Arctic Ocean under changing environmental conditions.
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