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
| dc.contributor.author | Barabach, Jan | |
| dc.contributor.author | Szczuciński, Witold | |
| dc.contributor.author | Kicińska, Ditta | |
| dc.contributor.author | Palińska, Zuzanna | |
| dc.contributor.author | Rachlewicz, Grzegorz | |
| dc.date.accessioned | 2024-01-17T09:07:31Z | |
| dc.date.available | 2024-01-17T09:07:31Z | |
| dc.date.issued | 2023-12 | |
| dc.description.abstract | 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. | |
| dc.identifier.citation | Barabach, J., Szczuciński, W., Kicińska, D., Palińska, Z., Rachlewicz, G., 2023: 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. Geographia Polonica 96 (4), 405-430. DOI: 10.7163/GPol.0262. | |
| dc.identifier.doi | http://doi.org/10.7163/GPol.0262 | |
| dc.identifier.uri | https://hdl.handle.net/10593/27583 | |
| dc.language.iso | en | |
| dc.publisher | Institute of Geography and Spatial Organization Polish Academy of Sciences | |
| dc.rights | Attribution 4.0 International | en |
| dc.subject | Speleology | |
| dc.subject | Speleologia | |
| dc.subject | cryosphere | |
| dc.subject | kriosfera | |
| dc.subject | cave | |
| dc.subject | jaskinia | |
| dc.subject | ice cave | |
| dc.subject | jaskinia lodowa | |
| dc.subject | Western Tatras | |
| dc.subject | Tatry Zachodnie | |
| dc.subject | Tatra Mountains | |
| dc.subject | Tatry | |
| dc.subject | history of cave research | |
| dc.subject | historia badań jaskiń | |
| dc.subject | climate change | |
| dc.subject | zmiana klimatu | |
| dc.subject | ice mass balance | |
| dc.subject | blians masy lodu | |
| dc.subject | cave climate | |
| dc.subject | klimat jaskini | |
| dc.subject | Jaskinia Lodowa w Ciemniaku | |
| dc.subject | Ice Cave in Ciemniak | |
| dc.subject | cave ice | |
| dc.subject | lód jaskiniowy | |
| dc.subject | Late Holocene | |
| dc.subject | późny holocen | |
| dc.subject | cave exploration history | |
| dc.subject | historia eksploracji jaskiń | |
| dc.subject | cave ice genesis | |
| dc.subject | powstawanie lodu jaskiniowego | |
| dc.subject | cave ice climate record | |
| dc.subject | zapis paleoklimatu w lodzie jaskiniowym | |
| dc.subject | environmental change record | |
| dc.subject | zapis zmian środowiskowych | |
| dc.subject | climate warming impact | |
| dc.subject | skutki zmiany klimatu | |
| dc.title | 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 | |
| dc.type | info:eu-repo/semantics/article |