Titlebook: Bioclimatology and Natural Hazards; Katarína Střelcová (Faculty of Forestry),Csaba Mát Book 2009 Springer Science+Business Media B.V. 2009

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pericardium

GUEER

What Climate Can We Expect in Central/Eastern Europe by 2071–2100?2007), the key processes influencing the European climate can be summarized as follows: (i) water vapour transport from low to high latitudes has increased; (ii) variation of atmospheric circulation has changed on interannual as well as longer time scales; (iii) snow cover during winter has reduced

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BALK

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Some Facts on Extreme Weather Events Analysis in Slovakiathe IPCC (2001) report there was for the first time a discussion on a possible change in the shape of distribution curves of individual climatic phenomena, specifically the change in probability densities in the time series from different periods. The basic alternatives of shift of distribution curv

CLAIM

Wind Risk Assessment in Urban Environments: The Case of Falling Trees During Windstorm Events in Lis-Branco 2007). Trees have a moderating effect on the urban microclimate and improve the physical, biological and chemical aspects of the urban environment, namely by reducing the urban ‘heat island’ effect (Alcoforado 1992), by acting as a barrier against strong wind channelling (Lopes 2003), by pro

Synapse

Ozone Air Pollution in Extreme Weather Situation – Environmental Risk in Mountain Ecosystems15-day long heat wave with record temperatures and unusually persistent high-ozone concentrations was observed in Europe during August 2003 (Vautard et al. 2005). Special meteorological situation favored the progressiveaccumulation of ozone.

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Physiological Drought – How to Quantify it?ictive. Definition of drought from EncyclopediaWikipedia says ‘A drought is an extended period of months or years when a region notes a deficiency in its water supply’. According to Multilingual Technical Dictionary (ICID 1996), drought is ‘a sustained period of time, with insufficient precipitation

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