Record low Antarctic sea-ice linked to more frequent storms

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Photo by Torsten Dederichs on Unsplash
Photo by Torsten Dederichs on Unsplash

In 2023 the sea-ice levels in the oceans surrounding Antarctica reached new lows, falling by as much as 80% in some areas, and UK research has found these low levels of sea-ice changed the interactions between the ocean and the atmosphere, increased the frequency of storms. The authors say repeated low ice cover in subsequent winters will strengthen these impacts and are likely to lead to profound changes as far away as the tropics and the Northern Hemisphere.

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From: Springer Nature

Climate change: Antarctic sea-ice losses drive storm formation (N&V)

Recent record lows in Antarctic sea-ice extent have led to increases in the frequency of storms over the newly ice-free ocean, reports a paper published in Nature this week. In 2023, the concentration of sea ice in the oceans surrounding Antarctica fell by as much as 80% in some areas, leading to increased heat transfer from the ocean to the atmosphere, which is associated with increased storminess. The findings reveal the wider climate system impacts of sea-ice loss.

The reduction of sea ice in Antarctica can lead to ocean warming, a weakening of the carbon sink in the Southern Ocean and population reductions in penguin colonies. While researchers have observed a large-scale reduction in sea ice beginning in 2016, 2023 set a record low sea-ice concentration beginning in February, with 2.33 million square kilometres of ice failing to regrow by June — twice that of  the previous lowest June value.

Simon Josey and colleagues analysed satellite and near-ocean surface atmospheric data and found three areas of anomalously low sea-ice cover in winter 2023, with the strongest reductions being 80% relative to the 1991–2020 June–July average. This loss of ice is accompanied by an increase in the amount of heat being released into the atmosphere from the ocean, with some areas experiencing double the amount of heat loss compared to pre-2015 values. This increased heat loss is associated with increases in the frequency of storms, with the authors calculating up to an additional 7 days of storms occurring over the areas with substantial reductions in ice. In addition, changes in the transfer of heat may have implications for how the ocean circulates, specifically how the Antarctic bottom water — a deep layer of water with high density and cold temperatures in the Southern Ocean — may absorb and store heat and carbon dioxide.

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Organisation/s: National Oceanography Centre, UK
Funder: Financing for this study has been provided by the UK Natural Environment Research Council (NERC) and the European Union’s Horizon 2020 research and innovation programme under grant agreement no. 821001 SO-CHIC. A.J.S.M. was also supported by OCEAN:ICE, which is co-funded by the European Union, Horizon Europe Funding Programme for research and innovation under grant agreement no. 101060452, BIOPOLE National Capability Multicentre Round 2 funding from the NERC (grant no. NE/W004933/1 and by UK Research and Innovation). A.T.B. and J.M. were also supported by NERC ATLANTIS (NE/Y005589/1). We thank K. F. Gunn and B. Sinha for useful comments.
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