Abstract
Regional climatological effects of global warming may be recognized not only in shifts of mean temperature and precipitation but also in the frequency and intensity changes of different climate extremes. A joint WMO-CCl (World Meteorological Organization Commission for Climatology)/CLIVAR (a project of the World Climate Research Programme addressing Climate Variability and Predictability) working group formed in 1998 on climate change detection (Karl et al. 1999); one of its task groups aimed to identify climate extreme indices (Peterson et al. 2002) and completed a climate extreme analysis on all parts of the world where appropriate data were available (Frich et al. 2002).
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Pongrácz, R., Bartholy, J., Gelybó, G., Szabó, P. (2009). Detected and Expected Trends of Extreme Climate Indices for the Carpathian Basin. In: Střelcová, K., et al. Bioclimatology and Natural Hazards. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-8876-6_2
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