Modeling the Trooz Glacier’s movement using air temperature data and satellite SAR observations in 2015–2022

Abstract

Under climate change, the world ocean's level rises rapidly due to the melting of grounded glaciers. A significant input to this process comes from the discharges of the Arctic and Antarctic Ice Sheets. In recent decades, significant efforts have been undertaken to study polar glaciers (Lemos et al., 2018; Stocker-Waldhuber et al., 2019; Friedl et al., 2021) and iceflow velocity changes. The study regions cover Ar ctic Canada, Greenland, some individual European territories, including Svalbard, in the north, and the Antarctic Peninsula in the south.