Jaskinia Lodowa w Ciemniaku (Ice Cave in Ciemniak), Western Tatra, Poland - over a century-long investigations of climate warming-caused degradation of subterranean ice mass

cris.lastimport.scopus2025-10-23T06:58:10Z
dc.abstract.enJaskinia Lodowa w Ciemniaku (Ice Cave in Ciemniak), in the Tatra Mountains (Tatry), is believed to host the largest subterranean ice mass in Poland. It has been known for over a century, however, the onset of its scientific investigations dates back to 1922, when Tadeusz and Stefan Zwoliński mapped it. Since then, it has become one of the best-known caves in Poland. It was described in over a hundred scientific and popular science papers. They include findings of international importance, e.g. works related to radioisotopes, ice-mass balance and age. However, some of the questions asked a century ago are still partly unanswered. One may wonder if they will be delivered before climate warming causes the largest ‘cave glacier’ in Poland to disappear.
dc.affiliationWydział Inżynierii Środowiska i Inżynierii Mechanicznej
dc.affiliation.instituteKatedra Melioracji, Kształtowania Środowiska i Gospodarki Przestrzennej
dc.contributor.authorBarabach, Jan
dc.contributor.authorSzczuciński, Witold
dc.contributor.authorKicińska, Ditta
dc.contributor.authorPalińska, Zuzanna
dc.contributor.authorRachlewicz, Grzegorz
dc.date.access2025-06-24
dc.date.accessioned2025-10-07T11:42:22Z
dc.date.available2025-10-07T11:42:22Z
dc.date.copyright2023-11
dc.date.issued2023
dc.description.abstract<jats:p>Jaskinia Lodowa w Ciemniaku (Ice Cave in Ciemniak), in the Tatra Mountains (Tatry), is believed to host the largest subterranean ice mass in Poland. It has been known for over a century, however, the onset of its scientific investigations dates back to 1922, when Tadeusz and Stefan Zwoliński mapped it. Since then, it has become one of the best-known caves in Poland. It was described in over a hundred scientific and popular science papers. They include findings of international importance, e.g. works related to radioisotopes, ice-mass balance and age. However, some of the questions asked a century ago are still partly unanswered. One may wonder if they will be delivered before climate warming causes the largest ‘cave glacier’ in Poland to disappear.</jats:p>
dc.description.accesstimeat_publication
dc.description.bibliographyil., bibliogr.
dc.description.financepublication_nocost
dc.description.financecost0,00
dc.description.if1,1
dc.description.number4
dc.description.points100
dc.description.versionfinal_published
dc.description.volume96
dc.identifier.doi10.7163/GPol.0262
dc.identifier.eissn2300-7362
dc.identifier.issn0016-7282
dc.identifier.urihttps://sciencerep.up.poznan.pl/handle/item/5246
dc.identifier.weblinkhttps://www.geographiapolonica.pl/article/item/13809.html
dc.languageen
dc.relation.ispartofGeographia Polonica
dc.relation.pages405-430
dc.rightsCC-BY
dc.sciencecloudnosend
dc.share.typeOPEN_JOURNAL
dc.subject.enspeleology
dc.subject.encryosphere
dc.subject.enWestern Tatras
dc.subject.enhistory of cave research
dc.subject.enice cave
dc.subject.enclimate change
dc.titleJaskinia Lodowa w Ciemniaku (Ice Cave in Ciemniak), Western Tatra, Poland - over a century-long investigations of climate warming-caused degradation of subterranean ice mass
dc.typeJournalArticle
dspace.entity.typePublication
oaire.citation.issue4
oaire.citation.volume96