Recession and Ice Surface Elevation Changes of Baranowski Glacier and Its Impact on Proglacial Relief (King George Island, West Antarctica)

• Published in: Geosciences
• Main Authors: Joanna Sziło, Robert Józef Bialik
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2018
• Subjects: deglaciation; proglacial landform; ice surface elevation changes; terrestrial laser scanning; Geology; QE1-996.5; Antarctic; Antarctic Peninsula; Baranowski Glacier; King George Island; Shallow Bay; The Antarctic; West Antarctica; Antarc*; Antarctica
• Online Access: https://doi.org/10.3390/geosciences8100355; https://doaj.org/article/eee20e5dc1384a218853f57c0d02964b

Glacial forefields areas are dynamic landscapes, and due to the glacier frontal position changes, they are sensitive to climatic fluctuations. The results of the analysis of aerial photos, satellite imagery, archival maps, and terrestrial laser scanning surveys are presented. These investigations reveal that the ice surface decreased during the period 1989–2001, when almost the entire current forefield was already uncovered. Moreover, it is shown that, since 1969, there has been a relationship between the changes in air temperature and the changes of the annual front position rate of Baranowski Glacier. Specifically, the results demonstrate that during the cooling observed for the Antarctic Peninsula Regions since 2000, there is a deceleration of the recession rate and ice surface elevation changes of Baranowski Glacier. It is also shown that the fluctuation of the areal extent of the glacier as well as ice surface elevation changes are closely associated with proglacial relief. Moreover, it is shown that the difference in the retreat of the northern and southern tongue of the glacier can be explained by the presence of relatively warm water in the shallow bay, which can enhance the melting process of the northern part. In addition, existence of long flutes and crevasse fill ridges on the analyzed forefield of Baranowski Glacier suggest that the former episodes of its surge, which could happen at least in the northern part of the forefield and middle part of the southern forefield of the glacier.