Hint: Use Kepler's laws of planetary motion.
step 1: Find the angular velocities at the apogee and perigee.
Consider the diagram. Let m be the mass of the earth, vp, va be the velocity of the earth at perigee and apogee respectively. Similarly, ωp and ωa are corresponding angular velocities.
Angular momentum and areal velocity are constant as the earth orbits the sun.
At perigee, r2pωp=r2aωa at apogee ...(i)
If a is the semi-major axis of the earth's orbit, then rp=a(1-e) and ra=a(1+e) ...(ii)
∴ ωpωa=(1+e1-e)2, e=0.0167 [From Eqs. (i) and (ii)]
∴ ωpωa=1.0691
Let ω be angular speed which is the geometric mean of ωp and ωa and corresponds to mean solar day,
∴ (ωpω)(ωωa)=1.0691
∴ ωpω=ωωa=1.034
Step 2: Find if it explains the variation of the length of the day during year.
If ω corresponding to 1° per day (mean angular speed), then ωp=1.034° per day and ωa=0.967° per day. Since, 361°=24 h, mean solar day, we get 361.034° which corresponds to 24 h, 8.14"(8.1" longer) and 360.967° corresponds to 23 h 59 min 52"(7.9" smaller). This does not explain the actual variation of the length of the day during the year.