This last interaction with the interface refracts the light back into the atmosphere, but it also diffracts a portion of the light as illustrated below. The beam, still traveling inside the water droplet, is once again refracted as it strikes the interface for a third time. As a light wave traveling through the atmosphere encounters a droplet of water, as illustrated below, it is first refracted at the water-to-air interface, then it is reflected as it again encounters the interface. The amount of diffraction depends on the wavelength of light, with longer wavelengths being diffracted at a greater angle than shorter ones (in effect, red light are diffracted at a higher angle than is blue and violet light). We can often observe pastel shades of blue, pink, purple, and green in clouds that are generated when light is diffracted from water droplets in the clouds. A good example of this is the diffraction of sunlight by clouds that we often refer to as a silver lining, illustrated in Figure 1 with a beautiful sunset over the ocean. This phenomenon can also occur when light is “bent” around particles that are on the same order of magnitude as the wavelength of the light. The parallel lines are actually diffraction patterns. As the fingers approach each other and come very close together, you begin to see a series of dark lines parallel to the fingers. A very simple demonstration of diffraction of waves can be conducted by holding your hand in front of a light source and slowly closing two fingers while observing the light transmitted between them.
0 Comments
Leave a Reply. |
AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |