6533b7ddfe1ef96bd1275176

RESEARCH PRODUCT

Subglacial topography and thickness of ice caps on the Argentine Islands

Jurijs JeškinsJānis KarušsMāris KrievānsAnatolii ChernovKristaps Lamsters

subject

010506 paleontologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeologyGlacierOceanography01 natural sciencesGeological structureIce thicknessPrevailing windsArchipelagoIce capsDigital surfaceGeomorphologyEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciences

description

AbstractThis study presents the first subglacial topography and ice thickness models of the largest ice caps of the Argentine Islands, Wilhelm Archipelago, West Antarctica. During this study, ground-penetrating radar was used to map the thickness and inner structure of the ice caps. Digital surface models of all studied islands were created from aerial images obtained with a small-sized unmanned aerial vehicle and used for the construction of subglacial topography models. Ice caps of the Argentine Islands cover ~50% of the land surface of the islands on average. The maximum thickness of only two islands (Galindez and Skua) exceeds 30 m, while the average thickness of all islands is only ~5 m. The maximum ice thickness reaches 35.3 m on Galindez Island. The ice thickness and glacier distribution are mainly governed by prevailing wind direction from the north. This has created the prominent narrow ice ridges on Uruguay and Irizar islands, which are not supported by topographic obstacles, as well as the elongated shape of other ice caps. The subglacial topography of the ice caps is undulated and mainly dependent on the geological structure and composition of magmatic rocks.

https://doi.org/10.1017/s0954102019000452