The thermal regime of ice pits of the Boreč hill
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41210%2F16%3A71854" target="_blank" >RIV/60460709:41210/16:71854 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
The thermal regime of ice pits of the Boreč hill
Original language description
The ecological stability of the sites with stenoec organisms is important factor for maintaining them at given location. Phonolite system of the Boreč hill creates a unique labyrinth of vents. Thermal anomalies occur during the year in the fissure system and create specific microclimate. Flow direction is given by the temperature gradient inside and outside of the system. The lower part of fissure system is located in the debris fields, while the upper part on top of the hill. Phonolite rocks are cooled down by air streaming from the debris fields during the winter. Direction of the air flow changes in the spring and summer. The cold air is exhaled from these vents on the lower parts of system and creates ice pits with the typical vegetation.
Czech name
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Czech description
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Classification
Type
D - Article in proceedings
CEP classification
DG - Atmospheric sciences, meteorology
OECD FORD branch
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Result continuities
Project
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Continuities
S - Specificky vyzkum na vysokych skolach
Others
Publication year
2016
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Article name in the collection
Mendel and Bioclimatology
ISBN
978-80-7509-397-4
ISSN
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e-ISSN
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Number of pages
7
Pages from-to
404-410
Publisher name
Mendel University in Brno
Place of publication
Brno
Event location
Brno
Event date
Sep 3, 2014
Type of event by nationality
WRD - Celosvětová akce
UT code for WoS article
000382229900043