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NCERT Exemplar · Q37

Q.Earth's orbit is an ellipse with eccentricity 0.0167. Thus, earth's distance from the sun and speed as it moves around the sun varies from day to day. This means that the length of the solar day is not constant through the year. Assume that earth's spin axis is normal to its orbital plane and find out the length of the shortest and the longest day. A day should be taken from noon to noon. Does this explain variation of length of the day during the year?

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Because Earth moves faster near perihelion and slower near aphelion (Kepler's second law), the extra rotation Earth must make each day to bring the Sun back overhead is slightly larger near perihelion and slightly smaller near aphelion. Working through the numbers, the solar day is about 7.9 seconds longer than average at perihelion and about 7.9 seconds shorter than average at aphelion — a total swing of roughly 16 seconds. This is far too small to explain the large day-length changes we notice through the seasons; those come from Earth's axial tilt, not from orbital eccentricity.

Why a solar day isn't simply Earth's rotation period

A solar day (noon to noon) is the time for the Sun to return to the same position in the sky, as seen from a fixed point on Earth. Because Earth also moves along its orbit while it spins, it must rotate slightly more than one full turn (relative to the distant stars) to bring the Sun back overhead — the extra bit of rotation needed each day equals the angle Earth has swept along its orbit in that time.

If Earth's orbital speed were constant (a circular orbit), that extra angle would be the same every day, and every solar day would be exactly the same length. But Earth's real orbit is a slightly eccentric ellipse (e=0.0167e=0.0167), so by Kepler's second law (equal areas in equal times), Earth moves fastest at perihelion (closest to the Sun, around early January) and slowest at aphelion (farthest, around early July). That means the extra angle to sweep each day is bigger near perihelion and smaller near aphelion — so the solar day itself is longer near perihelion and shorter near aphelion.

Setting up the sizes involved

Let n=2π/Tyearn=2\pi/T_{year} be Earth's mean orbital angular speed, and let ωs\omega_s be Earth's (constant) spin rate relative to the stars. Because Earth completes about one extra rotation per year just from orbiting the Sun, ωs\omega_s and nn are related by ωs−n≈365.25 n\omega_s - n \approx 365.25\,n (in other words, over the roughly 365.25 solar days in a year, the mean solar day exactly averages out to Dmean=2π/(ωs−n)=86400D_{mean}=2\pi/(\omega_s-n)=86400 s).

By conservation of angular momentum (r2θ˙=r^2\dot\theta= constant) with rP=a(1−e)r_P=a(1-e) and rA=a(1+e)r_A=a(1+e), and keeping only first-order terms in the small eccentricity e=0.0167e=0.0167, the orbital angular speed at the two extremes works out to

θ˙P≈n(1+2e),θ˙A≈n(1−2e)\dot\theta_P \approx n(1+2e), \qquad \dot\theta_A \approx n(1-2e)

so the orbital rate swings by ±2ne\pm2ne around its mean value nn.

From orbital-rate swing to solar-day-length swing

The solar day length is D=2π/(ωs−θ˙)D=2\pi/(\omega_s-\dot\theta). A small deviation δ=θ˙−n\delta=\dot\theta-n in the orbital rate produces a fractional change in DD of

ΔDDmean≈δωs−n=δ365.25 n\frac{\Delta D}{D_{mean}} \approx \frac{\delta}{\omega_s-n} = \frac{\delta}{365.25\,n}

At perihelion, δP=2ne\delta_P=2ne, so

ΔDPDmean=2ne365.25 n=2e365.25=2×0.0167365.25≈9.15×10−5\frac{\Delta D_P}{D_{mean}} = \frac{2ne}{365.25\,n} = \frac{2e}{365.25} = \frac{2\times0.0167}{365.25} \approx 9.15\times10^{-5}

ΔDP≈86400×9.15×10−5≈7.9 s\Delta D_P \approx 86400\times9.15\times10^{-5} \approx 7.9\text{ s}

By the same calculation with the opposite sign at aphelion, ΔDA≈−7.9\Delta D_A\approx-7.9 s.

The result …

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