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A. Mie Scattering B. Formed as sunlight is refracted by hexagonal plate- like ice crystals with diameters larger than 30 micrometers where they are oriented with their flat faces 1. Rainbows 2. Upside down image horizontal. C. A layer of very warm air near the ground refracts the light from the sky nearly into a U-shaped bend. D. Occur when raindrops responsible for the main rainbow are much uniform in size. E. Diffraction of sunlight in clouds produce a multitude of colors. F. It is about 10° further out from the antisolar point than the primary bow, is about twice as wide, and has its colors reversed. 3. Blue skies on a clear sunny day 4. White appearance of clouds 5. Halos 6. Mirages 7. Yellowish-red sunset G. High concentration of particles slightly larger than air molecules (like smoke, dust, and pollutants), the shorter and intermediate wavelengths of light (violet, blue and yellow) are scattered away H. Refraction by ice crystals associated with thin, level clouds that hexagonal crystals are randomly oriented I. Diffraction of cloud droplets J. Concave mirror K. Scattering of shorter wavelengths of light (violet and blue) L. Rayleigh scattering M. It is formed between about 40°, and 42° from the antisolar point where the light path involves refraction and a single reflection inside the water droplet. N. Color by subtraction O. Sunlight is refracted as it enters a raindrop, which causes the different wavelengths (colors) of visible light to separate. 8. Orange-red appearance of sun high- 9. Sundogs 10. Coronas 11. Cloud iridescence 12. Primary rainbow 13. Secondary rainbow 14. Supernumerary bows 15. Red shirt or cloth is red

A. Mie Scattering B. Formed as sunlight is refracted by hexagonal plate- like ice crystals with diameters larger than 30 micrometers where they are oriented with their flat faces 1. Rainbows 2. Upside down image horizontal. C. A layer of very warm air near the ground refracts the light from the sky nearly into a U-shaped bend. D. Occur when raindrops responsible for the main rainbow are much uniform in size. E. Diffraction of sunlight in clouds produce a multitude of colors. F. It is about 10° further out from the antisolar point than the primary bow, is about twice as wide, and has its colors reversed. 3. Blue skies on a clear sunny day 4. White appearance of clouds 5. Halos 6. Mirages 7. Yellowish-red sunset G. High concentration of particles slightly larger than air molecules (like smoke, dust, and pollutants), the shorter and intermediate wavelengths of light (violet, blue and yellow) are scattered away H. Refraction by ice crystals associated with thin, level clouds that hexagonal crystals are randomly oriented I. Diffraction of cloud droplets J. Concave mirror K. Scattering of shorter wavelengths of light (violet and blue) L. Rayleigh scattering M. It is formed between about 40°, and 42° from the antisolar point where the light path involves refraction and a single reflection inside the water droplet. N. Color by subtraction O. Sunlight is refracted as it enters a raindrop, which causes the different wavelengths (colors) of visible light to separate. 8. Orange-red appearance of sun high- 9. Sundogs 10. Coronas 11. Cloud iridescence 12. Primary rainbow 13. Secondary rainbow 14. Supernumerary bows 15. Red shirt or cloth is red

College Physics
College Physics
11th Edition
ISBN:9781305952300
Author:Raymond A. Serway, Chris Vuille
Publisher:Raymond A. Serway, Chris Vuille
Chapter1: Units, Trigonometry. And Vectors
Section: Chapter Questions
Problem 1CQ: Estimate the order of magnitude of the length, in meters, of each of the following; (a) a mouse, (b)...
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1. Rainbows 2. Upside down image A. Mie Scattering B. Formed as sunlight is refracted by hexagonal plate- like ice crystals with diameters larger than 30 micrometers where they are oriented with their flat faces horizontal. C. A layer of very warm air near the ground refracts the light from the sky nearly into a U-shaped bend. D. Occur when raindrops responsible for the main rainbow are much uniform in size. E. Diffraction of sunlight in clouds produce a multitude of colors. F. It is about 10° further out from the antisolar point than the primary bow, is about twice as wide, and has its colors reversed. 3. Blue skies on a clear sunny day 4. White appearance of clouds 5. Halos 6. Mirages 7. Yellowish-red sunset G. High concentration of particles slightly larger than air molecules (like smoke, dust, and pollutants), the shorter and intermediate wavelengths of light (violet, blue and yellow) are scattered away 8. Orange-red appearance of sun high- H. Refraction by ice crystals associated with thin, level clouds that hexagonal crystals are randomly oriented I. Diffraction of cloud droplets J. Concave mirror K. Scattering of shorter wavelengths of light (violet and blue) L. Rayleigh scattering M. It is formed between about 40°, and 42° from the antisolar point where the light path involves refraction and a single reflection inside the water droplet. N. Color by subtraction O. Sunlight is refracted as it enters a raindrop, which causes the different wavelengths (colors) of visible light to separate. 9. Sundogs 10. Coronas 11. Cloud iridescence 12. Primary rainbow 13. Secondary rainbow 14. Supernumerary bows 15. Red shirt or cloth is red
Transcribed Image Text:1. Rainbows 2. Upside down image A. Mie Scattering B. Formed as sunlight is refracted by hexagonal plate- like ice crystals with diameters larger than 30 micrometers where they are oriented with their flat faces horizontal. C. A layer of very warm air near the ground refracts the light from the sky nearly into a U-shaped bend. D. Occur when raindrops responsible for the main rainbow are much uniform in size. E. Diffraction of sunlight in clouds produce a multitude of colors. F. It is about 10° further out from the antisolar point than the primary bow, is about twice as wide, and has its colors reversed. 3. Blue skies on a clear sunny day 4. White appearance of clouds 5. Halos 6. Mirages 7. Yellowish-red sunset G. High concentration of particles slightly larger than air molecules (like smoke, dust, and pollutants), the shorter and intermediate wavelengths of light (violet, blue and yellow) are scattered away 8. Orange-red appearance of sun high- H. Refraction by ice crystals associated with thin, level clouds that hexagonal crystals are randomly oriented I. Diffraction of cloud droplets J. Concave mirror K. Scattering of shorter wavelengths of light (violet and blue) L. Rayleigh scattering M. It is formed between about 40°, and 42° from the antisolar point where the light path involves refraction and a single reflection inside the water droplet. N. Color by subtraction O. Sunlight is refracted as it enters a raindrop, which causes the different wavelengths (colors) of visible light to separate. 9. Sundogs 10. Coronas 11. Cloud iridescence 12. Primary rainbow 13. Secondary rainbow 14. Supernumerary bows 15. Red shirt or cloth is red
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