A. 舗gstrom, in his paper "Teleconnections of Climatic Changes im Present Time" uas demonstrated the relationship between the changes of temperature and variation of atmospheric circulation by the oretical means and statistical method. According to his theory that in all localities, where the temperature field is such, that an increase in the circu-lation means an increase also in the difference between energy of advection intr, duced and energy taken away, we will find an lucre ase in circulation correspond to a rise in temper-ature and vice versa.