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
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Institute of Geography and Spatial Organization Polish Academy of Sciences
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WA51_276513_r2023-t96-no4_G-Polonica-Barabach.pdf
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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.
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Speleology , Speleologia , cryosphere , kriosfera , cave , jaskinia , ice cave , jaskinia lodowa , Western Tatras , Tatry Zachodnie , Tatra Mountains , Tatry , history of cave research , historia badań jaskiń , climate change , zmiana klimatu , ice mass balance , blians masy lodu , cave climate , klimat jaskini , Jaskinia Lodowa w Ciemniaku , Ice Cave in Ciemniak , cave ice , lód jaskiniowy , Late Holocene , późny holocen , cave exploration history , historia eksploracji jaskiń , cave ice genesis , powstawanie lodu jaskiniowego , cave ice climate record , zapis paleoklimatu w lodzie jaskiniowym , environmental change record , zapis zmian środowiskowych , climate warming impact , skutki zmiany klimatu
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.
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