Abstract. Arctic landfast sea ice has undergone substantial changes in recent
decades, affecting ice stability and including potential impacts on ice
travel by coastal populations and on industry ice roads. We present a novel
approach for evaluating landfast sea ice stability on a pan-Arctic scale
using Synthetic Aperture Radar Interferometry (InSAR). Using Sentinel-1
images from spring 2017, we discriminate between bottomfast, stabilized, and
nonstabilized landfast ice over the main marginal seas of the Arctic Ocean
(Beaufort, Chukchi, East Siberian, Laptev, and Kara seas). This approach
draws on the evaluation of relative changes in interferometric fringe
patterns. This first comprehensive assessment of Arctic bottomfast sea ice
extent has revealed that most of the bottomfast sea ice is situated around
river mouths and coastal shallows. The Laptev and East Siberian seas dominate
the aerial extent, covering roughly 4100 and 5100 km2, respectively. These seas also contain the largest
extent of stabilized and nonstabilized landfast ice, but are subject to the
largest uncertainties surrounding the mapping scheme. Even so, we demonstrate
the potential for using InSAR for assessing the stability of landfast ice in
several key regions around the Arctic, providing a new understanding of how
stability may vary between regions. InSAR-derived stability may serve for
strategic planning and tactical decision support for different uses of
coastal ice. In a case study of the Nares Strait, we demonstrate that
interferograms may reveal early-warning signals for the breakup of stationary
sea ice.