 Radarsat, two imagery collected from 2015-2016 to 2019-2020 was used to quantify and characterize the variability in motion and discharge of major ice masses in the Queen Elizabeth Islands, with most glacier-experiencing little variation in flow speeds and dynamic thinning being attributed to pulse and surge processes. However, exceptions include Trinity and Wycombe Glacier and Belcher Glacier, which indicate continued acceleration by distinct processes. The average ice discharge to the ocean for the QEI over the observation period was 2.78 plus or minus 0.52 Gt1, with 5.0% of it being channeled through the Trinity Wycombe Glacier basin alone. The results provide a comprehensive record of ice motion and discharge from the QEI between 2008 and 2020. This article was authored by Wesley Van Wychern, David Burgess, Will Koptsky, and others. We are article.tv, links in the description below.