Abstract. As Arctic sea ice extent continues to decline, remote sensing
observations are becoming even more vital for the monitoring and
understanding of sea ice. Recently, the sea ice community has entered a new
era of synthetic aperture radar (SAR) satellites operating at C-band with
the launch of Sentinel-1A in 2014 and Sentinel-1B (S1) in 2016 and the
RADARSAT Constellation Mission (RCM) in 2019. These missions represent five
spaceborne SAR sensors that together routinely cover the pan-Arctic sea ice
domain. Here, we describe, apply, and validate the Environment and Climate
Change Canada automated sea ice tracking system (ECCC-ASITS) that routinely
generates large-scale sea ice motion (SIM) over the pan-Arctic domain using
SAR images from S1 and RCM. We applied the ECCC-ASITS to the incoming image
streams of S1 and RCM from March 2020 to October 2021 using a total of
135 471 SAR images and generated new SIM datasets (7 d 25 km and 3 d
6.25 km) by combining the image stream outputs of S1 and RCM (S1 + RCM).
Results indicate that S1 + RCM SIM provides more coverage in the Hudson Bay,
Davis Strait, Beaufort Sea, Bering Sea, and directly over the North Pole
compared to SIM from S1 alone. Based on the resolvable S1 + RCM SIM grid
cells, the 7 d 25 km spatiotemporal scale is able to provide the most
complete picture of SIM across the pan-Arctic from SAR imagery alone, but
considerable spatiotemporal coverage is also available from 3 d 6.25 SIM
products. S1 + RCM SIM is resolved within the narrow channels and inlets of
the Canadian Arctic Archipelago, filling a major gap from coarser-resolution
sensors. Validating the ECCC-ASITS using S1 and RCM imagery against buoys
indicates a root-mean-square error (RMSE) of 2.78 km for dry ice conditions
and 3.43 km for melt season conditions. Higher speeds are more apparent with
S1 + RCM SIM as comparison with the National Snow and Ice Data Center
(NSIDC) SIM product and the Ocean and Sea Ice Satellite Application Facility
(OSI SAF) SIM product indicated an RMSE of u=4.6 km d−1 and v=4.7 km d−1
for the NSIDC and u=3.9 km d−1 and v=3.9 km d−1 for OSI SAF. Overall,
our results demonstrate the robustness of the ECCC-ASITS for routinely
generating large-scale SIM entirely from SAR imagery across the pan-Arctic
domain.