Skip to content
NCERT Exemplar · Q28

Q.Mean solar day is the time interval between two successive noon when sun passes through zenith point (meridian). Sidereal day is the time interval between two successive transit of a distant star through the zenith point (meridian). By drawing appropriate diagram showing earth's spin and orbital motion, show that mean solar day is four minutes longer than the sidereal day. In other words, distant stars would rise 4 minutes early every successive day. (Hint: you may assume circular orbit for the earth).

Telangana TsbieShort· 5mImportance★★★★★est
85% · 57/67 Questions
🔒 Locked · start free trial →

You're viewing a preview — the full solution, concept, methods & PYQ mapping are locked.

Start your 14-day free trial to unlock the full solution →

Because Earth both spins on its axis and orbits the Sun, it must rotate slightly more than 360° to bring the Sun back to the meridian. This extra rotation takes about 4 minutes, making the solar day longer than the sidereal day.

Why the two days differ

A sidereal day measures one complete rotation of Earth relative to the distant stars—a full 360°. A mean solar day measures the time between successive noons, when the Sun crosses your local meridian. If Earth only rotated and did not orbit, these would be identical. But Earth simultaneously moves along its orbit around the Sun, so after one 360° spin the Sun has not yet returned to the meridian; Earth must rotate a little extra to "catch up" to the Sun. That extra rotation is what adds roughly 4 minutes.

The key insight is that in one day Earth travels about 1° along its orbit (since 360°/365.25≈1°360°/365.25 \approx 1° per day), and rotating through that additional 1° takes 1360\frac{1}{360} of a sidereal day.

Step-by-step derivation

  1. Set up the geometry.

    Imagine Earth at position A on day 1, with the Sun, Earth's center, and a point P on Earth's surface aligned so that the Sun is directly overhead at P (local noon). A distant star S lies in the same direction.

  2. One sidereal day later.

    Earth spins exactly 360° relative to the stars. Point P again points toward star S. Call this moment tsidt_{\text{sid}}. The sidereal day is complete.

  3. Earth has also moved in its orbit.

    During that same time tsidt_{\text{sid}}, Earth has traveled a small arc along its orbit. Because Earth takes roughly 365.25 days to complete one orbit of 360°, in one day it moves through an angle

θ≈360°365.25≈0.9856°≈1°.\theta \approx \frac{360°}{365.25} \approx 0.9856° \approx 1°.

  1. The Sun is no longer on the meridian.

    After the 360° spin, point P is again aligned with the distant star, but the Sun now lies about 1° behind in the sky (to the east, in Earth's orbital direction). To bring the Sun back to the meridian—to reach the next noon—Earth must rotate an additional ≈1°\approx 1°.

  2. Time for the extra rotation.

    One full 360° rotation takes one sidereal day, TsidT_{\text{sid}}. Rotating an extra 1° takes

Δt≈1°360° Tsid=Tsid360.\Delta t \approx \frac{1°}{360°} \, T_{\text{sid}} = \frac{T_{\text{sid}}}{360}.

  1. Relate sidereal and solar days. The mean solar day is

Tsol=Tsid+Δt=Tsid(1+1360)=Tsid361360.T_{\text{sol}} = T_{\text{sid}} + \Delta t = T_{\text{sid}} \left(1 + \frac{1}{360}\right) = T_{\text{sid}} \frac{361}{360}.

  1. Calculate the 4-minute difference. The sidereal day is about 23 hours 56 minutes 4 seconds =86 164= 86\,164 s. The extra fraction is Δt=86 164360≈239.3 s≈3.99 min≈4 min.\Delta t = \frac{86\,164}{360} \approx 239.3 \text{ s} \approx 3.99 \text{ min} \approx 4 \text{ min}. …

Unlock everything free for 14 days

  • Full step-by-step solutions
  • Concept-first explanations
  • Methods, shortcuts & mistakes
  • PYQ mapping + timed mock tests

Full access for 14 days. No credit card required.