Unprecedented Beaufort Sea ice loss in late summer 2021 and its relationship to an extended period of unusually stormy weather
Bibliographic Data
| ID | 15544879 |
|---|---|
| Authors | Thomas J Ballinger (0000-0002-8722-1927, University of Alaska Fairbanks, corresponding author), Peter M Finocchio (0000-0002-3987-6224, Naval Postgraduate School), V A Alexeev (0000-0003-3519-2797, University of Alaska Fairbanks), Igor V Polyakov (0000-0001-5912-8074, University of Alaska Fairbanks), James D Doyle (0000-0003-2941-2132, Naval Postgraduate School), Matthew G Fearon (0000-0002-2123-6528, Monterey Technologies (United States)), Linette Boisvert (0000-0003-4778-4765, Goddard Space Flight Center), Chelsea Parker (0000-0001-8026-6957, Goddard Space Flight Center) |
| Year | 2025 |
| Volume | 20 |
| Issue | 11 |
| Pages | 114067-114067 |
| Publication date | 2025-10-22 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Environmental Research Letters (JOURNAL) |
| Journal identifiers | ISSN: 1748-9326 • E-ISSN: 1748-9326 |
| Publisher | IOP Publishing (PUBLISHER • GB) |
| DOI | 10.1088/1748-9326/ae1626 |
| OpenAlex | W4415449589 |
| Language | EN |
| References cited | 39 |
Previous case studies have linked cyclone-induced atmospheric forcing and/or upper-ocean processes to notable Arctic sea ice loss events in the summers of 2012 and 2016. This study examines a more recent and noteworthy case in late summer 2021 in which substantial sea ice loss followed a period of surface meteorological extremes in the Beaufort Sea region of the Arctic. We focus on the period from mid-August to mid-September 2021 that coincided with the Office of Naval Research THINICE Pilot Field Campaign and investigate stormy and windy conditions with respect to air-sea processes impacting sea ice conditions. We find that during the stormy first half of the campaign, cyclone-induced energy fluxes into the marginal ice zone and surrounding waters preconditioned the ice pack for more rapid melt later in the campaign. The second half of the campaign, in contrast, was marked by non-cyclone wind events that enhanced turbulent (namely sensible) heat fluxes into the ice and upper ocean that increased melt. Moreover, this latter period had enhanced advection of the Beaufort Sea ice pack into above-freezing waters, increasing bottom melt to >1 cm d −1 over the remainder of the campaign. While findings are shown to vary by surface type and at relatively small (i.e. ice-floe) scales, insights are offered on the roles of late summer coupled processes on rapid ice loss events in today’s Arctic environment
Advection · Antarctic sea ice · Arctic · Arctic ice pack · Arctic sea ice decline · Cryosphere · Drift ice · Period (music · Sea ice · Arctic and Antarctic ice dynamics · Arctic and Russian Policy Studies · Methane Hydrates and Related Phenomena
| Highly cited | No |
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