Rescaled range analysis of the annual mean surface air temperatures at
7 meteorological stations in Hungary for the period of 1901-1991 indi
cates that the considered temperatures are fractals with a mean fracta
l dimension of 1.23 +/- 0.01. This value compares favourably with the
fractal dimensions of other climatic records, both on small time scale
of 10-100 years and for time spans 10(3)-10(6) years. Possibly such f
ractal dimensions are characteristic of climate change over the whole
spectral range of 10(3) to 10(6) years. If this assumption becomes con
firmed through analysis of a wider set of climatic records, long-range
climatic prediction (in statistical sense) on different time scales w
ill appear feasible.