Minimal change of thermal continentality in Slovakia within the period 1961–2013
Thermal continentality plays an important role not only in the basic characterisation of the climate in particular regions but also in the phytogeographic distribution of plants and ecosystem formation. Due to ongoing climate change, questions surrounding the changes of thermal continentality are ve...
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doaj-2bb6bcaa10bb443da9f557cd1a1427882020-11-24T22:33:23ZengCopernicus PublicationsEarth System Dynamics2190-49792190-49872016-08-017373574410.5194/esd-7-735-2016Minimal change of thermal continentality in Slovakia within the period 1961–2013J. Vilček0J. Škvarenina1J. Vido2P. Nalevanková3R. Kandrík4J. Škvareninová5Department of Geography and Applied Geoinformatics, University of Presov, 17. novembra 15, 080 01, Presov, SlovakiaDepartment of Natural Environment, Faculty of Forestry, Technical University in Zvolen, T.G. Masaryka 24, 960 53 Zvolen, SlovakiaDepartment of Natural Environment, Faculty of Forestry, Technical University in Zvolen, T.G. Masaryka 24, 960 53 Zvolen, SlovakiaDepartment of Natural Environment, Faculty of Forestry, Technical University in Zvolen, T.G. Masaryka 24, 960 53 Zvolen, SlovakiaDepartment of Natural Environment, Faculty of Forestry, Technical University in Zvolen, T.G. Masaryka 24, 960 53 Zvolen, SlovakiaDepartment of Applied Ecology, Faculty of Ecology and Environmental Sciences, Technical University in Zvolen, T.G. Masaryka 24, 960 53 Zvolen, SlovakiaThermal continentality plays an important role not only in the basic characterisation of the climate in particular regions but also in the phytogeographic distribution of plants and ecosystem formation. Due to ongoing climate change, questions surrounding the changes of thermal continentality are very relevant. Therefore, the aim of this study is to investigate the characteristics of thermal continentality and its temporal changes in the Slovak Republic between the years of 1961 and 2013. The study was carried out on several meteorological stations selected in respect to the geographical and geomorphological heterogeneity of Slovakia. Our results show that the continentality of Slovakia increased in the period 1961 to 2013; however, this trend is not significant. These non-significant trends are confirmed at all the stations. Nevertheless, it is necessary to be aware of this signal, especially because these changes could cause changes in ecosystem formation in future.http://www.earth-syst-dynam.net/7/735/2016/esd-7-735-2016.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
J. Vilček J. Škvarenina J. Vido P. Nalevanková R. Kandrík J. Škvareninová |
spellingShingle |
J. Vilček J. Škvarenina J. Vido P. Nalevanková R. Kandrík J. Škvareninová Minimal change of thermal continentality in Slovakia within the period 1961–2013 Earth System Dynamics |
author_facet |
J. Vilček J. Škvarenina J. Vido P. Nalevanková R. Kandrík J. Škvareninová |
author_sort |
J. Vilček |
title |
Minimal change of thermal continentality in Slovakia within the period
1961–2013 |
title_short |
Minimal change of thermal continentality in Slovakia within the period
1961–2013 |
title_full |
Minimal change of thermal continentality in Slovakia within the period
1961–2013 |
title_fullStr |
Minimal change of thermal continentality in Slovakia within the period
1961–2013 |
title_full_unstemmed |
Minimal change of thermal continentality in Slovakia within the period
1961–2013 |
title_sort |
minimal change of thermal continentality in slovakia within the period
1961–2013 |
publisher |
Copernicus Publications |
series |
Earth System Dynamics |
issn |
2190-4979 2190-4987 |
publishDate |
2016-08-01 |
description |
Thermal continentality plays an important role not only in the basic
characterisation of the climate in particular regions but also in the
phytogeographic distribution of plants and ecosystem formation. Due to
ongoing climate change, questions surrounding the changes of thermal
continentality are very relevant. Therefore, the aim of this study is to
investigate the characteristics of thermal continentality and its temporal
changes in the Slovak Republic between the years of 1961 and 2013. The study
was carried out on several meteorological stations selected in respect to
the geographical and geomorphological heterogeneity of Slovakia. Our results
show that the continentality of Slovakia increased in the period 1961 to
2013; however, this trend is not significant. These non-significant trends
are confirmed at all the stations. Nevertheless, it is necessary to be aware
of this signal, especially because these changes could cause changes in
ecosystem formation in future. |
url |
http://www.earth-syst-dynam.net/7/735/2016/esd-7-735-2016.pdf |
work_keys_str_mv |
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