the Thermal stream, capacity of a bark. The communication analysis

you are: the Thermal stream, capacity of a bark

For the communication analysis between thermal stream Q and modern vertical movements V simple correlation with correlation factor rq, v was used. Values fluctuate from practically zero correlation for Sredne-Russian height (zQiy=0,05) to the expressed correlation 0,65 for caucasus. In the areas designated by letters and, g, d, and, to, the thermal stream decreases with raising increase. It will be co-ordinated with the results received Harnishem. On the contrary, the areas designated by letters in, e, z, l, m, differ increase of vertical movements with increase in a thermal stream. This result coincides with the conclusions received by us earlier. It is important to notice, that if not the area of the l which is carrying out a role of a basis for the analysis in last mentioned articles the positive factor of regress would be the characteristic tektonicheski young mountain belts. It confirms legitimacy of division of all area on subdistricts. It is quite probable, that interrelation between a thermal stream and dynamics of the terrestrial surface which is a consequence of dynamics of a bark and a cloak, it is supervised by other geophysical and tectonic phenomena of studied area. The positive or negative factor of correlation cannot be extended to all area. To accept this or that factor of correlation it is possible only taking into account other geophysical data.