Preprints
https://doi.org/10.5194/egusphere-2026-3512
https://doi.org/10.5194/egusphere-2026-3512
17 Jul 2026
 | 17 Jul 2026
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

A comprehensive TLS-based framework for cave ice monitoring under adverse surface conditions: application at Scărișoara Ice Cave

Jozef Šupinský, Aurel Perşoiu, Michaela Nováková, Michal Gallay, and Ján Kaňuk

Abstract. Rapid degradation of cryospheric components requires reliable quantification of volumetric change to understand the leading processes and mechanisms behind the loss of ice. However, such monitoring in cave systems, a particularly complex morphological and climatic environment, remains methodologically challenging due to irregular geometry, limited accessibility, and increasingly dynamic ice-surface conditions. This study presents a comprehensive terrestrial laser scanning (TLS) data-processing framework from noise assessment, surface reconstruction, 3D volumetric change computation and error propagation as a transferable methodology for reliable monitoring of cave ice change even under suboptimal data acquisition conditions. The framework is demonstrated at Scărișoara Ice Cave (Romania) using three annual campaigns acquired with pulse-based and phase-shift scanners under conditions ranging from optimal dry and frozen surfaces to widespread meltwater presence. Scanner-specific noise assessment on different ice surface types reveals pronounced range, intensity and incidence angle dependent errors, demanding an efficient filtering strategy that reduces point cloud dispersion. A hybrid Poisson–MeshFix reconstruction strategy effectively fills meltwater-induced data gaps, reducing modelling error by up to five times. Multiresolution modelling tests show that 5 cm resolution provides an optimal balance between volumetric precision and computational efficiency with errors under 1 % compared to finer resolution models. Comparison of conventionally applied 2.5D change detection and 3D approach reveals ~20 % volumetric discrepancy, confirming that full 3D analysis is essential in such geometrically complex settings. The results reveal a cumulative ice loss of 1521 ± 65 m³ over three years, with heterogeneous spatial patterns controlled by cave morphology and drip-water distribution. Our data clearly shows that omitting any of the evaluated processing steps would greatly bias the volume estimates.

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Jozef Šupinský, Aurel Perşoiu, Michaela Nováková, Michal Gallay, and Ján Kaňuk

Status: open (until 28 Aug 2026)

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Jozef Šupinský, Aurel Perşoiu, Michaela Nováková, Michal Gallay, and Ján Kaňuk
Jozef Šupinský, Aurel Perşoiu, Michaela Nováková, Michal Gallay, and Ján Kaňuk
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Short summary
Rapid loss of cave ice demands reliable quantification of volumetric change, yet irregular geometry, limited access, and dynamic melt surfaces make this challenging. We present a transferable terrestrial laser scanning workflow, from noise assessment through surface reconstruction to three-dimensional change and error propagation, robust under suboptimal acquisition. At Scărișoara Ice Cave, Romania, it revealed a loss of 1521 cubic metres in three years, controlled by morphology and drip water.
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