Methodological approaches to survey complex ice cave environments - the case of Dobšiná (Slovakia)

dc.contributor.authorPukanská, Katarína
dc.contributor.authorBartoš, Karol
dc.contributor.authorGašinec, Juraj
dc.contributor.authorPašteka, Roman
dc.contributor.authorZahorec, Pavol
dc.contributor.authorPapčo, Juraj
dc.contributor.authorBella, Pavel
dc.contributor.authorAndrássy, Erik
dc.contributor.authorDušeková, Laura
dc.contributor.authorBobíková, Diana
dc.contributor.authorKseňak, Ľubomír
dc.date.accessioned2026-06-08T10:41:47Z
dc.date.available2026-06-08T10:41:47Z
dc.date.issued2024
dc.description.abstractIntroduction Dobšiná; Ice Cave (Slovakia) has attracted the attention of many researchers since its discovery more than 150 years ago. Although the cave is located outside the high-mountain area, it hosts one of the largest volumes of underground perennial ice. The topographic mapping of this unique UNESCO Natural Heritage site has led to several historical surveys. In the last decades of rapid climate change, this natural formation has been subject to rapid changes that are dynamically affecting the shape of the ice body. Increased precipitation, the rise in year-round surface temperatures, and the gravity cause significant shape changes in the ice filling.Methods This paper describes modern technological tools to comprehensively survey and evaluate interannual changes in both the floor and wall of the underground ice body. Technologies such as digital photogrammetry, in combination with precise digital tacheometry and terrestrial laser scanning, make it possible to detect ice accumulation and loss, including the effect of sublimation due to airflow, as well as sliding movements of the ice body to the lower part of the cave. To get a comprehensive model of the ice volume, geophysical methods (microgravimetry and ground penetrating radar) have been added to determine the thickness of the floor ice in the upper parts of the cave in the last 2 years.Results Between 2018 and 2023, the ice volume in certain sections of the cave decreased by up to 667 m(3), with notable reductions in ice thickness ranging from 0.3 to 0.9 m in areas like the Small Hall and Collapsed Dome. The study also detected dynamic changes, such as the widening of the ice tunnel by 20 cm in some sections, and a vertical ice wall in Ruffinyi's Corridor showed localized volume losses up to 9 m3 (between 2018 and 2023). Additional geophysical methods - microgravimetry and ground penetrating radar - revealed an average ice thickness ranging from 10 to 25 m.Discussion The paper not only highlights the current technological possibilities but also points out the limitations of these technologies and then sets out solutions with a proposal of technological procedures for obtaining accurate geodetic and geophysical data.
dc.description.firstpageart. no. 1484169
dc.description.sourceWeb of Science
dc.description.volume12
dc.identifier.citationFrontiers in Environmental Science. 2024, vol. 12, art. no. 1484169.
dc.identifier.doi10.3389/fenvs.2024.1484169
dc.identifier.issn2296-665X
dc.identifier.urihttp://hdl.handle.net/10084/158760
dc.identifier.wos001388487200001
dc.language.isoen
dc.publisherFrontiers Media S.A.
dc.relation.ispartofseriesFrontiers in Environmental Science
dc.relation.urihttps://doi.org/10.3389/fenvs.2024.1484169
dc.rights© 2024 Pukanská, Bartoš,Gašinec, Pašteka, Zahorec, Papčo, Bella, Andrássy, Dušeková, Bobíková and Kseňak.
dc.rights.accessopenAccess
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.subjectice cave
dc.subjectcryomorphological topography
dc.subjecttacheometry
dc.subjectphotogrammetry
dc.subjectlaser scanning
dc.subjectSLAM
dc.subjectmicrogravimetry
dc.subjectground penetrating radar
dc.titleMethodological approaches to survey complex ice cave environments - the case of Dobšiná (Slovakia)
dc.typearticle
dc.type.statusPeer-reviewed
dc.type.versionpublishedVersion
local.files.count1
local.files.size8218886
local.has.filesyes

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