Method and apparatus for modification of supercooled fog

A method for the reduction of supercooled fog that is restrained below an inversion layer, said method comprising

• (1) introducing liquid carbon dioxide through a nozzle into a supercooled fog from the ground while moving the nozzle along a line along the ground, the amount of liquid carbon dioxide introduced into the supercooled fog being sufficient to form ice crystals due to evaporation of supercooled fog droplets and subsequent formation of ice crystals;
• (2) generating sufficient heat from the formation of ice crystals to cause a slowly rising updraft that carries the ice crystals in a slowly rising plume from the bottom to the top of the supercooled fog;
• (3) diffusing and spreading the ice crystals horizontally near the top of the supercooled fog as a result of turbulent diffusion and buoyancy of the ice crystal plume at the bottom of the inversion layer;
• (4) gradually increasing the size of the ice crystals as they rise and diffuse into the supercooled fog such that the ice crystals fall through the underlying fog in a lateral extension of the plume formed in step (1);
• (5) inducing evaporation of supercooled fog droplets and crystallization of the evaporated fog droplets onto the ice crystals falling through the supercooled fog in the lateral extension, wherein additional heat is generated and causes a slowly rising updraft that is sufficient to carry the smaller ice crystals upwardly to the top of the supercooled fog;
• (6) spreading the smaller ice crystals horizontally near the top of the supercooled fog as a result of the buoyancy of the smaller ice crystals;
• (7) gradually increasing the size of the smaller ice crystals as they spread horizontally such that resulting ice crystals of increased size fall through the underlying supercooled fog in an ever expanding lateral extension of the plume formed in step (1).