以下の英語文を日本語に翻訳してください。
All the light in our daytime sky comes from the sun, and our sun produces light in many different colors. To understand this, just think of a prism.  White light enters, and a rainbow of colors exits. Our sun is like that. Its light may seem uniform but it is actually emitting many different colors.

Our sky though is not a mix of blue and red and green because the earth's atmosphere is sandwiched between the sun and us, getting in the way. Atmospheric gases and particles scatter the incoming colors, bouncing them in all different directions.  The amount of scattering increases as the wavelength of light decreases.  Red light which has a long wavelength is scattered much less than blue light which has a short wavelength. As blue is scattered more, it fills our daytime sky.

As the sun traverses the sky and moves low on the horizon, the light that reaches our eyes must actually travel further through the atmosphere.  This has the effect of completely bouncing away all the blue light.  We are left with the reds and yellows and oranges in wonderful mixture, making sunrises and sunsets so beautiful.
昼間の空の光はすべて太陽からやってくるもので、太陽はさまざまな色の光を作り出している。これを理解するには、プリズムを思い浮かべてほしい。白い光が入り、虹色の光が出る。太陽もそのようなものだ。でも、私たちの空は青と赤と緑が混在しているわけではない。大気中のガスや粒子は、入ってくる色を散乱させ、あらゆる方向に跳ね返す。散乱の量は、光の波長が短くなるほど多くなる。波長の長い赤色光は、波長の短い青色光よりも散乱量が少ない。波長の長い赤色光は、波長の短い青色光よりも散乱される量が少なく、青色光の方が散乱される量が多いため、日中の空は青色光でいっぱいになる。 その結果、青い光は完全に弾き飛ばされる。 その結果、赤や黄色やオレンジが混ざり合い、朝日や夕日がとても美しく見えるのだ。