The role of cross-polarization in producing high-resolution pan-Arctic sea ice motion from the RADARSAT Constellation Mission over several years

We introduce a new pan-Arctic Environment and Climate Change Canada (ECCC) HIgh-Resolution sea Ice Tracking System (HIRITS) operating with the RADARSAT Constellation Mission (RCM) HH and HV synthetic aperture radar (SAR) images resampled at a resolution of 80 m. The spacing between neighbour output vectors was often around 1 km. When combining HH and HV, the resulting ice displacements (over 2 h to 3.5 days) derived for June 1, 2022 – May 31, 2025 were in an excellent agreement with International Arctic Buoy Programme data with the overall root-mean square error (RMSE) of 1.48 km, and correlation of 0.996 for the x and y components. Ice motion vectors provided by HV had consistently greater tracking cross-correlation coefficients (with the average value of 0.56) than those derived from HH (average value of 0.45), implying a higher confidence. The RCM HH + HV ice motion agreed well with the existing passive microwave products from the National Snow and Ice Data Center (NSIDC) and Ocean and Sea Ice Satellite Application Facility (OSI SAF) with RMSEs of 4.19 km/d and 5.03 km/d respectively. We introduced an aggregated sea ice motion pan-Arctic gridded product at 2 km resolution that combines individual RCM ice motion products (HH and HV) derived over 3- and 7-day rolling time windows. A greater number of vectors was derived from HV compared to HH across the pan-Arctic domain, except for the situations where the HV signal is low, such as over smooth land fast ice. The new RCM HH + HV products generated since mid-May 2022 will substantially benefit various applications that require sea ice motion at high spatial resolution including accurate computation of sea ice deformation. • New pan-Arctic HIgh-Resolution Ice Tracking System (HIRITS) is introduced. • Pan-Arctic sea ice motion is derived from the RCM's HH and HV imagery. • RCM-derived ice motion agrees very well with buoy data over a 36-months period. • HV channel of RCM provides excellent added value to HH throughout an ice season.

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Publication Details

Journal
Remote Sensing of Environment
Published
2025-12-04
DOI
https://doi.org/10.1016/j.rse.2025.115175
Citations
1
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
1.30
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article

The role of cross-polarization in producing high-resolution pan-Arctic sea ice motion from the RADARSAT Constellation Mission over several years

Stephen Howell, Jean-François Lemieux, Mike Brady, Alexander S. Komarov et al.
1 citations
Remote Sensing of Environment
Arctic and Antarctic ice dynamics
1.30
article

The role of cross-polarization in producing high-resolution pan-Arctic sea ice motion from the RADARSAT Constellation Mission over several years

Stephen Howell, Jean-François Lemieux, Mike Brady, Alexander S. Komarov, Mathieu Plante
article en
1 citations

Abstract

We introduce a new pan-Arctic Environment and Climate Change Canada (ECCC) HIgh-Resolution sea Ice Tracking System (HIRITS) operating with the RADARSAT Constellation Mission (RCM) HH and HV synthetic aperture radar (SAR) images resampled at a resolution of 80 m. The spacing between neighbour output vectors was often around 1 km. When combining HH and HV, the resulting ice displacements (over 2 h to 3.5 days) derived for June 1, 2022 – May 31, 2025 were in an excellent agreement with International Arctic Buoy Programme data with the overall root-mean square error (RMSE) of 1.48 km, and correlation of 0.996 for the x and y components. Ice motion vectors provided by HV had consistently greater tracking cross-correlation coefficients (with the average value of 0.56) than those derived from HH (average value of 0.45), implying a higher confidence. The RCM HH + HV ice motion agreed well with the existing passive microwave products from the National Snow and Ice Data Center (NSIDC) and Ocean and Sea Ice Satellite Application Facility (OSI SAF) with RMSEs of 4.19 km/d and 5.03 km/d respectively. We introduced an aggregated sea ice motion pan-Arctic gridded product at 2 km resolution that combines individual RCM ice motion products (HH and HV) derived over 3- and 7-day rolling time windows. A greater number of vectors was derived from HV compared to HH across the pan-Arctic domain, except for the situations where the HV signal is low, such as over smooth land fast ice. The new RCM HH + HV products generated since mid-May 2022 will substantially benefit various applications that require sea ice motion at high spatial resolution including accurate computation of sea ice deformation. • New pan-Arctic HIgh-Resolution Ice Tracking System (HIRITS) is introduced. • Pan-Arctic sea ice motion is derived from the RCM's HH and HV imagery. • RCM-derived ice motion agrees very well with buoy data over a 36-months period. • HV channel of RCM provides excellent added value to HH throughout an ice season.

Remote Sensing of EnvironmentVol. 334
Environment and Climate Change Canada (CA)
Openalex Percentile: Top 16%
Arctic and Antarctic ice dynamics
1.30
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