ppt on atmospheric refraction

14
Atmospheric refraction Done By V.K.Ramdas XB 09

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Page 1: Ppt on atmospheric refraction

Atmospheric refraction

Done ByV.K.Ramdas

XB09

Page 2: Ppt on atmospheric refraction

Atmospheric refraction near the ground produce mirages and can make distant objects appear to shimmer or ripple, elevated or lowered , stretched or shortened with no mirage involved

Page 3: Ppt on atmospheric refraction

Shimmering of face

• When we sit around a campfire , the face of the person opposite to us appears to shimmer.

• This happens due to refraction of light. The rays of light reflected from the face of the person sitting opposite to us , on passing through hot air , gets refracted. Since hot air is rapidly moving and its optical density is continuously changing . Therefore the path of refracted rays also changes.

• This gives shimmering effect.

Page 4: Ppt on atmospheric refraction

Advanced sunrise and delayed sunset

• The sun is visible to us before the actual sunrise and after the sunset.

• The density of air near the surface of the earth is slightly higher. The rays of the sun coming through space enter at the top of the earth’s atmosphere and travel from rarer to denser medium.

• They bend slightly towards normal at each refraction and appear to come from apparent position of sun. Hence , sun appears to rise a few minutes before the actual rise . The same phenomenon applicable for delayed sunset as the sun continues to be seen a few minutes after it has actually set.

Page 5: Ppt on atmospheric refraction
Page 6: Ppt on atmospheric refraction

Apparent position and twinkling of stars

• The starlight on entering earth’s atmosphere undergoes refraction continuously before it reaches the observer.

• Since the refractive index of the earth’s atmosphere is gradually changing , the atmosphere bends the starlight towards the normal, and the apparent position of the star is slightly higher than its actual position.

• As the path of rays of the light coming from the stars goes on varying slightly , the apparent position of the star fluctuates and the amount of light entering the eye flickers.

Page 7: Ppt on atmospheric refraction
Page 8: Ppt on atmospheric refraction

Planets do not twinkle

• Planets are very close to us as compared to stars. This apparent position also changes with the change in the density of different layers of atmosphere. However , the size of their apparent image is still fairly large , such that it seldom falls outside the line of sight. Hence , they do not appear to twinkle.

Page 9: Ppt on atmospheric refraction

Sun appears bigger during sunset or sunrise

• If the sun (or moon ) is low above the horizon , the optical path of the light through the atmosphere is very long thus refraction is also maximum.

• Hence , apparent image of the sun is very much closer to the eye . Thus, it appears bigger.

Page 10: Ppt on atmospheric refraction

Sun appears flattened at sunrise or sunset but circular at noon

• At sunset and sunrise , the sun is near the horizon. The rays of light from the upper and lower edge of the sun bend unequally while travelling through the atmosphere. As a result of this phenomenon , the sun appears oval or flattened.

• At noon , the sun is overhead. The rays of light from the sun enter the atmosphere normally and do not bend. So the sun appears circular.

Page 11: Ppt on atmospheric refraction

PRINCIPLE OF

MIRAGE

Page 12: Ppt on atmospheric refraction

MIRAGE FORMED IN

DESERT

Page 13: Ppt on atmospheric refraction

Mirage• Warm air is less dense than cool air and the difference between them creates a

gradient in the refractive index of air. • Light from the sky at a shallow angle to the road is refracted making it appear as if

the sky is reflected by the road’s surface. • The mind interprets this as a pool of water on the road as water also reflects the sky.

Page 14: Ppt on atmospheric refraction

THE END