Detailed Monitoring of the Antarctic Marginal Ice Zone by Satellite Radar Altimeter Synergy—A Study of the Weddell Sea/Indian Ocean Sector in July 2017

Abstract The wave‐affected Marginal Ice Zones (MIZ) is a key region of air‐ice‐ocean interactions in the Southern Ocean (SO). However, challenges still remain for the large‐scale observation of the MIZ. In this study, we use four concurrent radar altimeters to retrieve the wave‐affected MIZ in the eastern Weddell Sea‐Indian Ocean sector, which was surveyed by an in situ campaign during July 2017. We show that a strong cyclone induced a 600 km‐wide MIZ in the eastern Weddell Sea, while in the Indian Ocean sector, MIZ width is generally 200 km throughout the month. The derived wave attenuation rate is closely related with both swell period and ice conditions. Moreover, we demonstrate that the MIZ width, combined with the incident swell power, serves as a proxy for ice thickness in the MIZ. The retrieval algorithms can be further applied to wave‐ice interaction studies and the construction of long‐term records of MIZs in the SO.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-11-20
DOI
https://doi.org/10.1029/2025gl115782
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
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article

Detailed Monitoring of the Antarctic Marginal Ice Zone by Satellite Radar Altimeter Synergy—A Study of the Weddell Sea/Indian Ocean Sector in July 2017

Lu Zhou, Clare Eayrs, Marcello Vichi, Alexander D. Fraser et al.
Geophysical Research Letters
Arctic and Antarctic ice dynamics
article

Detailed Monitoring of the Antarctic Marginal Ice Zone by Satellite Radar Altimeter Synergy—A Study of the Weddell Sea/Indian Ocean Sector in July 2017

Lu Zhou, Clare Eayrs, Marcello Vichi, Alexander D. Fraser, Shiming Xu, Siqi Liu, Xiaohui Cheng, Weixin Zhu
article en

Abstract

Abstract The wave‐affected Marginal Ice Zones (MIZ) is a key region of air‐ice‐ocean interactions in the Southern Ocean (SO). However, challenges still remain for the large‐scale observation of the MIZ. In this study, we use four concurrent radar altimeters to retrieve the wave‐affected MIZ in the eastern Weddell Sea‐Indian Ocean sector, which was surveyed by an in situ campaign during July 2017. We show that a strong cyclone induced a 600 km‐wide MIZ in the eastern Weddell Sea, while in the Indian Ocean sector, MIZ width is generally 200 km throughout the month. The derived wave attenuation rate is closely related with both swell period and ice conditions. Moreover, we demonstrate that the MIZ width, combined with the incident swell power, serves as a proxy for ice thickness in the MIZ. The retrieval algorithms can be further applied to wave‐ice interaction studies and the construction of long‐term records of MIZs in the SO.

Geophysical Research LettersVol. 52(22)
University of Tasmania (AU), Australian Antarctic Division (AU), Polar Research Institute of China (CN), University of Cape Town (ZA), Utrecht University (NL), Korea Polar Research Institute (KR), Tsinghua University (CN)
Openalex Percentile: Top 60%
Arctic and Antarctic ice dynamics
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Detailed Monitoring of the Antarctic Marginal Ice Zone by Satellite Radar Altimeter Synergy—A Study of the Weddell Sea/Indian Ocean Sector in July 2017 — Lu Zhou, Clare Eayrs, et al. · Geophysical Research Letters (2025) | TGRS Research Map | TGRS