Problem solved in full
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The colour the Sun peaks at and why a greenhouse works 5 steps
Find the colour the Sun peaks at, and then use the same one-line law to explain why a greenhouse works — and why night-vision cameras see warm bodies at all. Sun: T = 5772 K.
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Everything with a temperature radiates, and the wavelength it radiates most strongly at is inversely proportional to temperature. Hotter means bluer — that is the whole content of Wien’s law, and the constant is fixed by nature.
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Substitute the Sun’s effective temperature. The calculator above prints this figure, and it lands in green — near the middle of the visible band, and very close to where the human eye is most sensitive.
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The frequency follows immediately from the wave relation, and the tool prints this too.
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Now apply the identical law to something that is not a star: Earth’s surface at 288 K.
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Compare the two peaks. Same law, same constant, temperatures differing by a factor of 20 — so wavelengths differ by a factor of 20 in the other direction.
Answer
502 nm, in the green. Earth peaks at 10.06 μm, deep in the infrared, and that factor of twenty is the entire greenhouse mechanism: glass and CO₂ are transparent at half a micron and opaque at ten, so sunlight arrives freely and the re-radiated heat cannot leave by the same route. It is also why thermal cameras work in the dark — a 310 K body peaks near 9.4 μm and glows constantly at a wavelength your eye cannot see. One inverse proportionality, three unrelated-looking phenomena.
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References (2)
- The distribution whose maximum gives the displacement law: M. Planck, "Ueber das Gesetz der Energieverteilung im Normalspectrum." Annalen der Physik 309(3), 553–563, 1901.
- The value of the displacement constant b, and of h, c and k_B behind it: E. Tiesinga, P. J. Mohr, D. B. Newell and B. N. Taylor, "CODATA recommended values of the fundamental physical constants: 2018." Reviews of Modern Physics 93(2), 025010, 2021.