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Zmena klímy – možný dopad (nielen) na obyvateľstvo - Prohuman

Zmena klímy – možný dopad (nielen) na obyvateľstvo - Prohuman

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adiation since 1961 (IPCC, 2007). Increase of the atmospheric greenhouse gases<br />

concentration and enhanced atmospheric greenhouse effect is probably the<br />

only acceptable forcing factor and expla<strong>na</strong>tion for such development (IPCC, 2007).<br />

Variations in the air temperature series can be caused also by several <strong>na</strong>tural processes.<br />

Irregular atmospheric and oceanic circulation oscillations (ElNiňo, ENSO,<br />

NAO, AO, AAO) are the reasons of most of sudden inter-annual and inter-seaso<strong>na</strong>l<br />

deviations (Figs. 1–4). Daily and monthly temperature variations in small areas,<br />

like Slovakia, can be caused mostly by random changes in atmospheric circulation<br />

(synoptic causes)<br />

Figure 3. Annual averages of<br />

air temperature deviations<br />

(dT) from the 1961–1990<br />

mean in the Northern Hemisphere<br />

continents (solid line)<br />

and Global (dashed line) in<br />

1971–2010 (by CRU, 2012).<br />

Figure 4. Annual averages of<br />

air temperature deviations (dT)<br />

from the 1961–1990 mean in the<br />

Northern Hemisphere continents<br />

(solid line) and Global<br />

(dashed line) in 1880–2010 (by<br />

CRU, 2012).<br />

Air temperature projections and sce<strong>na</strong>rios until the 2100 show continuation of<br />

irregular increase by about 3°C (Fig. 5), this increase is nearly equally all year round.<br />

Variability of air temperature values (means and daily extremes) will not change<br />

significantly, but its impacts are supposed as more negative than before. Sudden decrease<br />

of air temperature after long series of relatively warm days may cause higher<br />

damages in the ecosystems and socio-economic sectors than frequent changes of<br />

93

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