optics val bennington october 2008. path of radiation (light) can be modified: reflected scattered...

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Optics Val Bennington October 2008

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Page 1: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Optics

Val Bennington

October 2008

Page 2: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Path of Radiation (Light)

Can be modified:

• Reflected

• Scattered

• Absorbed

Or path may remain the same:

• Transmitted

Page 3: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Reflection

• If reflected, all wavelengths hitting an object at one angle will be reflected along the same path

• Angle of incidence = Angle of reflection• Does not spread the colors of visible light!

Page 4: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Refraction - How Light is Scattered

• Separates different colors!!!• Path through object DEPENDS ON

WAVELENGTH !!!

Page 5: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Review on Visible Light

• Violets and blues are higher energy• Red has longest wavelength• Blue / violet has shortest wavelength

Page 6: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Snell’s Law

• Light slows when entering medium of higher refractive index

• This causes the path of the light ray to bend toward the normal

n1sin1 = n2sin2

Page 7: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Snell’s Law Continued…

n1sin1 = n2sin2

n depends on wavelength !

When exiting a medium, light bends AWAY from normal (reverse the ray directions)

Page 8: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Why is the sky Blue?

• The atmosphere scatters visible light, so we receive direct light (from the direction of the sun) and diffuse light (from all directions).

• The atmosphere more effectively scatters shorter wavelengths (blue) than longer wavelengths (red).

• Thus when the sun is high in the sky, away from the sun the sky appears blue.

• At sunset, sunlight must pass through a larger amount of atmosphere, enough so that red light is also scattered resulting in a red sky/clouds near the horizon.

Page 9: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Rainbows

Page 10: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Rainbows

• Notice that violet and blue light are most bent (scattered) in the raindrop

• Blue light and shorter wavelengths are MOST SCATTERED by raindrops and other aerosols in the atmosphere

• Red light is least bent or scattered

Page 11: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Rainbows cont.

Page 12: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Dispersion

• Light is dispersed when traveling through the raindrop

• In other words, colors are separated

• The path of each wavelength is changed, spreading the colors

Page 13: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Halos

• Light travels through ICE CRYSTALS when a halo is formed

• Ice crystals randomly oriented (not all facing one direction)

Page 14: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

• Sun’s rays bent 22˚

• Sun’s rays appear TO YOU to be coming from around the sun

Page 15: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Sundogs (mock suns)

• If ice crystals mostly or all oriented with flat faces horizontal, sundogs appear

Hand covers actual sun

Page 16: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Other Phenomena

• Mirages (due to temperature gradient)• Green Flash• Sun Pillar• Coronas• Glories• Broken Bow

Page 17: Optics Val Bennington October 2008. Path of Radiation (Light) Can be modified: Reflected Scattered Absorbed Or path may remain the same: Transmitted

Extra Credit• Up to five points to write a paragraph about one of: Sun Pillar, Coronas, Glories, Broken Bow, or Green Flash• Draw a diagram of the observer, the light source, and how the

light is bent, reflected, or scattered• Expect more than the couple sentences in the book, although

feel free to use the textbook as a start• Make sure to explain how and why the light is bent and why

light appears to be coming from a certain direction to the observer

• List references on your extra credit sheet (make sure if it is from the internet, that it is from a university or research website)

• Hand in your Extra Credit at start of class next week