Spring 2021 sea ice transport in the southern Beaufort Sea occurred during coastal-lead opening events

Abstract. Winds blew a record large portion of the Arctic's multiyear sea ice (MYI) into the southern Beaufort Sea (SBS) in winter 2021. From early March, a network of buoys from the Sea Ice Dynamic Experiment (SIDEx) tracked the MYI as it drifted across the SBS toward the Chukchi Sea. Transport was episodic as the consolidated ice pack interacted with coastal boundaries and repeatedly fractured. We investigated variability in 2021 MYI transport by relating in situ sea ice drift to remotely sensed coastal-lead opening events, which have been associated with increased ice drift speeds in winter. Daily ice concentration data show 10 opening events occurred throughout March and April 2021. Opening lasted 1–5 consecutive days as southeasterly winds pushed the SBS ice pack away from coastal boundaries. During opening, the ice pack abruptly accelerated and its response to wind forcing stabilized around free-drift conditions, drifting at 2.1 % of wind speeds (median rate of 13.7 km d−1). With this efficient wind-to-ice momentum transfer, nearly all (94 %) alongshore MYI transport in March–April 2021 occurred during opening events, which comprised just half of March–April days. Only 6 % of transport occurred during the other half of days without observed opening. On these days, the ice was mostly stationary (median of 1.7 km d−1 drift rate, 0.6 % of wind speeds) as northwesterly winds compressed the pack against the coast. Spatiotemporal discontinuities in ice–wind speed ratios were measured across several coastal leads that transected the SIDEx buoy network, providing direct observations of changes in the ice drift regime as coastal leads opened. These results quantify the disproportionate contribution of offshore and alongshore winds in breaking the SBS ice pack away from the coast, opening leads, and driving SBS ice transport during spring 2021, highlighting the critical role these episodic events play in consolidated-season sea ice drift.

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Publication Details

Journal
˜The œcryosphere
Published
2025-03-28
DOI
https://doi.org/10.5194/tc-19-1413-2025
Citations
1
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
1.30

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article

Spring 2021 sea ice transport in the southern Beaufort Sea occurred during coastal-lead opening events

Angela C. Bliss, MacKenzie E. Jewell, Jennifer Hutchings
1 citations
˜The œcryosphere
Arctic and Antarctic ice dynamics
1.30
article

Spring 2021 sea ice transport in the southern Beaufort Sea occurred during coastal-lead opening events

Angela C. Bliss, MacKenzie E. Jewell, Jennifer Hutchings
article en
1 citations

Abstract

Abstract. Winds blew a record large portion of the Arctic's multiyear sea ice (MYI) into the southern Beaufort Sea (SBS) in winter 2021. From early March, a network of buoys from the Sea Ice Dynamic Experiment (SIDEx) tracked the MYI as it drifted across the SBS toward the Chukchi Sea. Transport was episodic as the consolidated ice pack interacted with coastal boundaries and repeatedly fractured. We investigated variability in 2021 MYI transport by relating in situ sea ice drift to remotely sensed coastal-lead opening events, which have been associated with increased ice drift speeds in winter. Daily ice concentration data show 10 opening events occurred throughout March and April 2021. Opening lasted 1–5 consecutive days as southeasterly winds pushed the SBS ice pack away from coastal boundaries. During opening, the ice pack abruptly accelerated and its response to wind forcing stabilized around free-drift conditions, drifting at 2.1 % of wind speeds (median rate of 13.7 km d−1). With this efficient wind-to-ice momentum transfer, nearly all (94 %) alongshore MYI transport in March–April 2021 occurred during opening events, which comprised just half of March–April days. Only 6 % of transport occurred during the other half of days without observed opening. On these days, the ice was mostly stationary (median of 1.7 km d−1 drift rate, 0.6 % of wind speeds) as northwesterly winds compressed the pack against the coast. Spatiotemporal discontinuities in ice–wind speed ratios were measured across several coastal leads that transected the SIDEx buoy network, providing direct observations of changes in the ice drift regime as coastal leads opened. These results quantify the disproportionate contribution of offshore and alongshore winds in breaking the SBS ice pack away from the coast, opening leads, and driving SBS ice transport during spring 2021, highlighting the critical role these episodic events play in consolidated-season sea ice drift.

˜The œcryosphereVol. 19(3)
Goddard Space Flight Center (US), Oregon State University (US)
National Aeronautics and Space Administration, Office of Naval Research
Openalex Percentile: Top 25%
Arctic and Antarctic ice dynamics
1.30
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