Ice-free geomorphometry of Queen Maud Land, East Antarctica: 3. Belgica and Yamato (Queen Fabiola) Mountains
I.V. Florinsky, S.O. Zharnova

TL;DR
This study models and maps key topographic variables of ice-free regions in Queen Maud Land, East Antarctica, providing a detailed quantitative resource for diverse scientific research.
Contribution
It introduces a comprehensive geomorphometric modeling approach for two specific ice-free mountain areas using REMA data, creating a reproducible topographic atlas.
Findings
Detailed models of eleven morphometric variables for Belgica and Yamato Mountains.
Quantitative topographic maps useful for geological and ecological studies.
Reproducible methodology for Antarctic ice-free terrain analysis.
Abstract
Geomorphometric modeling and mapping of ice-free Antarctic areas can be applied for obtaining new quantitative knowledge about the topography of these unique landscapes and for the further use of morphometric information in Antarctic research. Within the framework of a project of creating a physical geographical thematic scientific reference geomorphometric atlas of ice-free areas of Antarctica, we performed geomorphometric modeling and mapping of two, partly ice-free mountainous areas of the eastern Queen Maud Land, East Antarctica. These include the Belgica Mountains and Yamato (Queen Fabiola) Mountains. As input data, we used two fragments of the Reference Elevation Model of Antarctica (REMA). For the two ice-free areas and adjacent glaciers, we derived models and maps of eleven, most scientifically important morphometric variables (i.e., slope, aspect, horizontal curvature, vertical…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsPolar Research and Ecology · Cryospheric studies and observations · Climate change and permafrost
