Ice in caves and its effect on thermal inversion and permafrost in the case of the Velika ledena jama v Paradani, Smrekova draga and neighbouring dolines
In the Velika ledena jama v Paradani, in the karstic blowholes on the slopes of Smrekova draga and in the nearby dolines I measured and interpreted air temperatures and the effect of the summer outflow of cold air from them into the surrounding area. In winter, cold air enters the cave, radically co...
| Published in: | Acta Carsologica |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
ZRC SAZU, Založba ZRC
2021
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| Subjects: | |
| Online Access: | https://ojs.zrc-sazu.si/carsologica/article/view/10495/9656 https://ojs.zrc-sazu.si/carsologica/article/view/10495/9669 https://ojs.zrc-sazu.si/carsologica/article/view/10495 |
| Summary: | In the Velika ledena jama v Paradani, in the karstic blowholes on the slopes of Smrekova draga and in the nearby dolines I measured and interpreted air temperatures and the effect of the summer outflow of cold air from them into the surrounding area. In winter, cold air enters the cave, radically cooling the entrance part of the cave, where for this reason there is permanent cave ice. The summertime circulation is reversed: emerging from the inner part of cave, which has an average temperature of around 4° C, is air which only when it transits through the sub-cooled entrance part is then cooled to around 1° C. This air comes to the surface and in the hollow at the cave entrance maintains a distinct thermal inversion during the warm part of the year. There is a similar air circulation and similar development of annual temperatures observed at the vents, where cave air emerges through rubble spread over cave entrances on slopes or at the bottom of dolines. The stable summer air temperatures of around 1° C in the vents where I conducted measurements indicate that underneath them there is also permafrost or sub-cooled rock and permanent ice. This is created and preserved, just like in the caves, due to the advection of cold air in winter. In Trnovski gozd, such karstic permafrost is found at an altitude of 1,100 m above sea level. The outflow of cold air from the vents in the summer, just like inside the cave, causes a distinct thermal inversion in dolines on the surface. V Veliki ledeni jami v Paradani, v dihalnikih na pobočjih Smrekove drage in v bližnjih vrtačah sem meril in interpretiral temperature zraka ter vpliv poletnega iztekanja hladnega zraka iz njih v okolico. V jamo pozimi vstopa mrzel zrak, ki močno podhladi vhodni del jame, kjer se zato ohranja stalni jamski led. Poletna cirkulacija je obrnjena; iz notranjega dela jame, ki ima povprečno temperaturo okrog 4° C piha zrak, ki se šele ob prehodu skozi podhlajeni vhodni del jame ohladi na okrog 1° C. Ta zrak izhaja na površje in v kotanji pri vhodu v ... |
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