rayleigh scattering वाक्य
उदाहरण वाक्य
मोबाइल
- Landsberg discovered the fine structure in Rayleigh scattering.
- This happens because of Rayleigh scattering, the same property that causes the sky to appear blue.
- It is first corrected for Rayleigh scattering and then subtracted from the Rayleigh corrected band 1.
- When illumination is indirect, Rayleigh scattering in the upper atmosphere will lead blue wavelengths to dominate.
- The statement that the sky is blue needs explaining that it is due to Rayleigh scattering.
- This is described by Rayleigh scattering, an effect that creates Earth's blue sky and red sunsets.
- Rayleigh scattering is much greater for blue light than for other colours due to its shorter wavelength.
- The blue of glacier ice is sometimes misattributed to Rayleigh scattering due to bubbles in the ice.
- The Sun is in fact white, but appears yellow through Earth's atmosphere due to atmospheric Rayleigh scattering.
- But when the sun is above the horizon anywhere, Rayleigh scattering makes the whole sky pretty bright.
- The Rayleigh scattering ( note spelling, everyone ) makes distant objects bluer, and yellow is complementary to blue.
- This simplest case is explained by Rayleigh scattering-and to understand that, you have to get into the math.
- Rayleigh scattering is already strong enough that outer space doesn't contribute much to the color of the sky.
- This is known as Rayleigh scattering.
- Rayleigh scattering and Mie scattering dominate what they see-just as they do for us down here on earth.
- Why wouldn't it, since Rayleigh scattering would favor that end of the spectrum when sunlight passes through more air?
- The Rayleigh scattering effect is therefore increased, removing virtually all blue light from the direct path to the observer.
- Another type of structural color results from the incoherent scattering of light, also known as Tyndall or Rayleigh scattering.
- Despite the strong wavelength dependence of Rayleigh scattering, its effect on sky glow for real light sources is small.
- The optical depth of the atmosphere can be divided into several components, ascribed to Rayleigh scattering, aerosols, and gaseous absorption.
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