Dew is a meteorological phenomenon in which the humidity in the air condenses in the form of drops due to a sudden decrease in temperature or contact with cold surfaces. It typically occurs at night and may reveal captivating images during sunrise when observed properly. In Fig. 1, I present a photograph of dew drops with the sun shining from behind. As observed, some of them display colors, a result of light refraction and observation angle, akin to the phenomenon seen in a rainbow.
© 2001-2024 Fundación Dialnet · Todos los derechos reservados