Fifty Years of Tidewater Glacier Surface Elevation and Retreat Dynamics along the South-East Coast of Spitsbergen (Svalbard Archipelago)

• Published in: Remote Sensing
• Main Authors: Jan Kavan, Guy D. Tallentire, Mihail Demidionov, Justyna Dudek, Mateusz C. Strzelecki
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2022
• Subjects: tidewater glaciers; surface elevation changes; glacier geometry; Svalbard; Science; Q; Svalbard Archipelago; glacier; Norwegian Polar Institute; Tidewater; Spitsbergen
• Online Access: https://doi.org/10.3390/rs14020354; https://doaj.org/article/44ffe7b88eda4eb19d222842dab5e617

Tidewater glaciers on the east coast of Svalbard were examined for surface elevation changes and retreat rate. An archival digital elevation model (DEM) from 1970 (generated from aerial images by the Norwegian Polar Institute) in combination with recent ArcticDEM were used to compare the surface elevation changes of eleven glaciers. This approach was complemented by a retreat rate estimation based on the analysis of Landsat and Sentinel-2 images. In total, four of the 11 tidewater glaciers became land-based due to the retreat of their termini. The remaining tidewater glaciers retreated at an average annual retreat rate of 48 m year −1 , and with range between 10–150 m year −1 . All the glaciers studied experienced thinning in their frontal zones with maximum surface elevation loss exceeding 100 m in the ablation areas of three glaciers. In contrast to the massive retreat and thinning of the frontal zones, a minor increase in ice thickness was recorded in some accumulation areas of the glaciers, exceeding 10 m on three glaciers. The change in glacier geometry suggests an important shift in glacier dynamics over the last 50 years, which very likely reflects the overall trend of increasing air temperatures. Such changes in glacier geometry are common at surging glaciers in their quiescent phase. Surging was detected on two glaciers studied, and was documented by the glacier front readvance and massive surface thinning in high elevated areas.