Abstract
McMurdo Sound sea ice can generally be partitioned into two regimes: (1) a stable fast-ice cover, forming south of approximately 77.6∘ S around March–April and then breaking out the following January–February, and (2) a more dynamic region north of 77.6∘ S that the McMurdo Sound and Ross Sea polynyas regularly impact. In 2019, a stable fast-ice cover formed unusually late due to repeated break-out events. We analyse the 2019 sea-ice conditions and relate them to a modified storm index (MSI), a proxy for southerly wind events. We find there is a strong correlation between the timing of break-out events and several unusually large MSI events.
Original language | English |
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Pages (from-to) | 4999–5006 |
Number of pages | 8 |
Journal | The Cryosphere |
Volume | 15 |
Issue number | 10 |
DOIs | |
Publication status | Published - 29 Oct 2021 |