Based on the atlas tables 2.2 to 2.6 of the mean precipitation heights of the years; and
hydrological half-years will also be the coefficient of variation of the annual and semi-annual
Precipitation levels of the period 1961-1990 calculated. In addition, the medium
Coefficient of variation of the individual months.
Since the behaviour of the temporal variability of precipitation is largely independent of the
Correction of the systematic measurement error, all calculations with the uncorrected
Precipitation heights are carried out. The grid field representation is smoothed to
Eliminate station extremes.
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