I. Introduction
Glaciers play an important role in the Earth’s climate system, and their monitoring and analysis are critical to understanding the impacts of climate change [1], [2]. Over the years, the field of glacier monitoring has witnessed an increased use of SAR technology [3]. SAR sensors operate irrespective of sunlight and weather conditions, enabling continuous monitoring. This all-weather, all-day capability is particularly advantageous in high mountain areas, where persistent and dense cloud cover presents challenges to traditional optical remote sensing techniques [4]. In addition, microwave signals from SAR can penetrate the surface of glaciers and provide valuable information about their internal structure and dynamics [5].