First arctic-wide assessment of SWOT swath altimetry with ICESat-2 over sea ice

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Authors: Felix L. Müller, Denise Dettmering, Florian Seitz
Cited by: 1
References: 21

Abstract

This study presents an Arctic-wide assessment of the Surface Water and Ocean Topography (SWOT) mission's swath observations of sea surface height (SSH). SWOT provides measurements in two-dimensional swaths and enables pixel-based height information with a resolution of 250 m up to a latitudinal limit of 78° N. Although SWOT doesn’t cover the central Arctic, it provides insights into SSH at an unprecedented spatial and temporal resolution. The quality of these innovative observations in such a challenging environment is evaluated through comparison with data from ICESat-2. Approximately one year of surface elevation data, collected between March 2023 and April 2024, is used at around 550 regionally distributed crossover locations, with measurements taken within 30 min. Sentinel-1 SAR imagery supports the comparisons if available. Visual comparisons of SWOT and ICESat-2 with Sentinel-1 backscatter (i.e. σ 0 ), converted to 8-bit grey-scale values, reveal clear coherence. However, small-scale surface features aren’t captured by SWOT as equally as by ICESat-2. The data shows absolute water level differences of about 5 cm, despite prior harmonisation of references and corrections. Differences of up to 50 cm can occur when comparing left- and right-hand SWOT swaths, mainly during winter and in areas with long sea ice coverage. This may be due to issues with the height correction from the crossover calibration. Quantitative point-by-point comparisons show mean standard deviations of about 8 cm for all surface types and 6 cm if restricted to ICESat-2-detected leads. Higher deviations are found during the early melting period between May and June, in the Canadian Archipelago and the Greenland Sea.

Fields of Study & Subjects

Arctic and Antarctic ice dynamics Oceanographic and Atmospheric Processes Climate change and permafrost

Publication details

Journal / source
˜The œcryosphere
Publisher
Copernicus GmbH
Volume
20
Issue
1
Pages
397–409
Publication date
20 January 2026
Language
EN