For bulk water samples, these conditions are described as «no man's land,» because ice
nucleates before such temperatures can be reached.
Not exact matches
Crossing this barrier enabled the liquid to propagate laterally across the surface in a stepwise fashion, often
nucleating from a central point
before zipping along the grooves and filling them.
Surface ice storms are also now a constant threat due to the chemical ice
nucleating elements reaching the surface
before solidifying.
With atmospheric conditions this warm, the chemically ice
nucleating elements often reach the ground level
before setting up as ice, thus creating extremely destructive «ice storms».