Stability of Dynamics of Humidifcation and Warmth Securing of Geo-systems
Criteria of stability of dynamics of humidifcation and warmth securing of geo-systems are revealed from the positions of physical geography process optimum. Grounded is steadiness of humidifcation and thermal content phase states in relation to equivalent parity of warmth and moisture, the latter being an organizing and stabilizing prime of natural and natural-and-anthropogenic systems. Thermodynamic stability within the cover of a group of Baikal, TransBaikal and Mongolian weather stations is estimated