Galileo Gallei measured the angular positions of the stars with his telescope. To adjust his telescope, he initially aimed at the Pole Star, which is always at the same position in the sky at an angle of α with the horizontal.
On a cold winter's night of − 3 ° C , he conducted his measurements inside his study room at 2 0 ° C . The starlight fell through his window and refracted twice on the glass. From his room, Polaris appeared at an angle of β with the horizon.
What is the angle difference δ = β − α between measurements inside and outside?
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Just like the website's name, brilliant solution! I couldn't have come up with this!
Amazing problem. Brilliant solution.
Amazing solution...
We can get to the answer slightly more easily as follows... sin α sin β = 1 + R ⋆ T 2 c p 1 + R ⋆ T 1 c p = 1 + 3 × 2 9 3 1 1 + 3 × 2 7 0 1 = 1 . 0 0 0 0 4 8 4 and so, writing β = α + δ , we have (with α ≈ . 4 5 ∘ ): cos δ + cot α sin δ cos δ + sin δ 2 cos ( 4 5 ∘ − δ ) 4 5 ∘ − δ δ = 1 . 0 0 0 0 4 8 4 = 1 . 0 0 0 0 4 8 4 = 1 . 0 0 0 0 4 8 4 = 4 4 . 9 9 7 2 2 2 6 8 5 ∘ = 2 . 7 7 3 1 5 × 1 0 − 3 ∘ = 9 . 9 8 ′ ′
However, since we are giving atmospheric pressure to 1 SF, and R ⋆ to 1 SF, the accuracy to which we have to calculate to identify δ seems beyond what is reasonable. All we can reasonably say with this data is that cos δ + sin δ = 1 , giving δ = 0 ∘ .
While we are at it, assuming that α = 4 5 ∘ is not globally true. At the North Pole, α = 9 0 ∘ , and α = 0 ∘ on the equator. 4 5 ∘ does work quite well for Italy, but it seems that required information of that nature should be provided in the question.
What is ρ ? Does it represent air density? Or is it "moles per unit volume?" If the former, don't you have to multiply the answer by (the atomic weight of air)/1000?
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Oh I get it. I didn't understand the term "specific gas constant." So I am wrong.
I took a lucky guess... This is totally out of my range
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The Snell's law for the refraction on the glass gives n outside sin α ⇒ β = n glass sin γ = n inside sin β = arcsin [ n inside n outside sin α ] with the refractive indices n glass of the glass pane as well as n inside and n outside of the air inside and outside. Although the air inside and outside has the same composition and pressure p ≈ 1 bar = 1 0 5 Pa , there is a difference in the temperature difference the density ρ . With the ideal gas law follows ⇒ p n = R ∗ ρ T ⇔ ρ = R ∗ T p = ε = 1 + χ = 1 + c ρ = 1 + R ∗ T c p Here we have use the fact that the air molecules show almost no magnetism at room temperature ( μ ≈ 1 ), so that the refractive index of the air is only determined by dielectric properties ( n = ε μ ≈ ε ). Therefore, β = arcsin [ n inside n outside sin α ] = arcsin [ 1 + R ∗ T inside c p 1 + R ∗ T outside c p sin α ] ≈ arcsin [ 1 + R ∗ T outside c p − R ∗ T inside c p sin α ] ≈ arcsin [ ( 1 + 2 1 R ∗ c p [ T outside 1 − T inside 1 ] ) sin α ] ≈ α + 1 − ( sin α ) 2 1 ⋅ 2 R ∗ c p [ T outside 1 − T inside 1 ] sin α Here we have taken advantage of the fact that the refractive index of air differs only slightly from 1, so we used the approximations 1 + x 1 1 + x ≈ 1 − x ≈ 1 + 2 1 x for x ≪ 1 and also made an linear Taylor expansion for the arcus sine.
For the calculation of the angle β we have to know the angle height α of the polar star. Venice lies at the latitude ϕ = 4 5 ∘ , so that the position of the polar star also results to α ≈ 4 5 ∘ , since this star is located at the north pole of the sky. Therefore, sin α = 2 1 and thus δ = β − α ≈ 2 R ∗ c p [ T outside 1 − T inside 1 ] = 2 ⋅ 3 0 0 1 0 − 3 ⋅ 1 0 5 [ 2 7 0 1 − 2 9 3 1 ] ≈ 4 . 8 ⋅ 1 0 − 5 rad ≈ 0 . 0 0 2 8 ∘ ≈ 1 0 ′ ′