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No significant correlation between the mean altitude for TBE and precipitation could be found.
During 1961 1979, the mean altitude for TBE varied between 180 m and 340 m above sea level.
The mean altitude for TBE in this period was significantly correlated with mean annual air temperature (Table 2).
This correlation indicates that the mean altitude for TBE positively responds to climate warming, with a lag of several years.
The closest correlation was detected between the mean altitude for TBE and mean annual air temperature of the 3 preceding years.
The observed rise in mean altitude for TBE corresponds with a mean ± SD rate of TBE ceiling (uppermost limit) rise of ≈5.4 ± 1.7 m yearly during the past 3 decades in the neighboring Czech Republic (2 ).
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However, during the following period, 1980 2004, the mean altitudes for TBE showed nonrandom variation over time.
Time series of mean altitudes for TBE showed random elevation, and statistical analysis showed no temporal trend.
A series of yearly mean altitudes for TBE was analyzed for correlations with mean yearly temperature and precipitation derived from 12 meteorologic stations throughout Slovakia.
We also calculated the mean altitude of sampling locations for each species in each bioregion (Table 3).
Rufiji District has an overall mean altitude of <500 metres.
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