fénycsóvák
Fénycsóvák, which translates to "light beams" in Hungarian, is a term that can refer to several distinct phenomena. In the context of meteorology, it specifically describes a meteorological optical phenomenon where sunlight is scattered by ice crystals in the atmosphere, creating visible beams of light. These beams often originate from a strong light source, such as the sun, and appear to radiate outwards. They are typically seen when the sun is low on the horizon, often during sunrise or sunset, and are more pronounced when the sky is partially obscured by clouds or other atmospheric particles that can scatter the light.
Beyond its meteorological definition, "Fénycsóvák" can also be used metaphorically in a broader sense to denote