“Humid snow”: at the intersection of physics, linguistics, and emotional landscape
The expression “humid snow” seems simple and domestic, but behind it lies a complex natural phenomenon with a clear physical basis, a rich palette of linguistic nuances, and a stable culturally-psychological image. It is not just a description of the weather, but a whole concept that connects scientific understanding of phase transitions of water with the aesthetics of transitional, indeterminate states.
1. Physics and meteorology: what is humid snow really?
From a scientific point of view, “humid snow” is a colloquial term for two closely related but different atmospheric phenomena. Their nature depends on the temperature of atmospheric layers.
Snow grains (graupel) or ice grains: This is a snowflake nucleus (ice crystal) that, as it falls through a layer of subcooled droplets in the cloud, becomes covered with frost, turning into soft, opaque, white grains with a diameter of 2-5 mm. They are easily compacted and already contain a lot of air and water. This is the classic “humid snow” that can be molded into snowballs.
Snow with partial melting (wet snow): This is ordinary snowflakes (complex ice crystals) that fall through a layer of air with a temperature above 0°C. They partially melt, losing their clear crystal structure, become wet, clump together into flakes, and, when reaching the ground, often form a heavy, damp mass. This type of snow is the one that causes icing and sticking to wires and branches, leading to serious accidents in power grids.
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