Abstract
The meteorological and bioclimatologic vocabulary defines the term drought (dryness) from several points of view. In principle, however, it is defined as the state of water deficit concerning soil, plants and atmosphere (Krevčmer 1980). The grounds underlying lack of moisture are complex and intricate. In countries with generally sufficient water supply, the dryness is considered a rare event or even a natural calamity.
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Škvarenina, J., Tomlain, J., Hrvol’, J., Škvareninová, J. (2009). Occurrence of Dry and Wet Periods in Altitudinal Vegetation Stages of West Carpathians in Slovakia: Time-Series Analysis 1951–2005. In: Střelcová, K., et al. Bioclimatology and Natural Hazards. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-8876-6_8
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