IOAA 2015, Теория, дълги задачи, английски — Задача 1

International Olympiad on Astronomy and Astrophysics 2015, Central Java - Indonesia — Long Problems

Внимание: Бележка към темата

The revised official marking scheme is primary. Earlier image-key questions and marking weights differ and are labelled separately. The revised key leaves problem 3(d) blank; the earlier distance derivation adds an assumption absent from the final question. Printed algebraic inconsistencies are retained.

Instruction — Theoretical Round
  1. Write your answer on the answer-sheet only. You can use more than one sheet for one problem. Please ask the organizer for the additional answer-sheets.

  2. Different problems should be done on different sheets.

  3. You can use your own calculator without program and graphic facility.

  4. You can ask the organizer for rough paper.

Astronomical and Physical Constants — 20150729
ConstantValue
Astronomical unit (AU)1.4960×1011 m1.4960\times10^{11}\ \mathrm m
Light year (ly)9.4605×1015 m=63 240 au9.4605\times10^{15}\ \mathrm m=63\,240\ \mathrm{au}
Parsec (pc)3.0860×1016 m=206 265 au3.0860\times10^{16}\ \mathrm m=206\,265\ \mathrm{au}
Jansky (Jy)10−26 W m−2 Hz−110^{-26}\ \mathrm{W\,m^{-2}\,Hz^{-1}}
1 Sidereal year365.2564 solar days
1 Tropical year365.2422 solar days
1 Calendar year365.2425 solar days
1 Sidereal day23h 56m 04s.09123^{\mathrm h}\ 56^{\mathrm m}\ 04^{\mathrm s}.091
1 Solar day24h 03m 56s.55524^{\mathrm h}\ 03^{\mathrm m}\ 56^{\mathrm s}.555 units of sidereal time
1 Å10−10 m10^{-10}\ \mathrm m
1 erg10−7 J10^{-7}\ \mathrm J
1 dyne10−5 N10^{-5}\ \mathrm N
Mass of Earth5.9736×1024 kg5.9736\times10^{24}\ \mathrm{kg}
Mean radius of Earth6.371×106 m6.371\times10^6\ \mathrm m
Equatorial radius of Earth6.378×106 m6.378\times10^6\ \mathrm m
Mean velocity of Earth on its orbit29.783 km s−129.783\ \mathrm{km\,s^{-1}}
Mass of Moon7.3490×1022 kg7.3490\times10^{22}\ \mathrm{kg}
Radius of Moon1.737×106 m1.737\times10^6\ \mathrm m
Mass of Jupiter1.89813×1027 kg1.89813\times10^{27}\ \mathrm{kg}
Mean Earth – Moon distance3.844×108 m3.844\times10^8\ \mathrm m
Mass of Sun1.98892×1030 kg1.98892\times10^{30}\ \mathrm{kg}
Radius of Sun6.96×108 m6.96\times10^8\ \mathrm m
Effective temperature of the Sun5780 K
Luminosity of the Sun3.96×1026 J s−13.96\times10^{26}\ \mathrm{J\,s^{-1}}
Solar constant1366 W m−21366\ \mathrm{W\,m^{-2}}
Brightness of the Sun in V-band−26.8 mag.
Absolute brightness of the Sun in V-band4.75 mag.
Absolute bolometric brightness of Sun4.72 mag.
Angular diameter of the Sun30′
Speed of light in vacuum (c)2.9979×108 m s−12.9979\times10^8\ \mathrm{m\,s^{-1}}
Gravitational constant (G)6.6738×10−11 N m2 kg−26.6738\times10^{-11}\ \mathrm{N\,m^2\,kg^{-2}}
Boltzmann constant (k)1.381×10−23 m kg s−2 K−11.381\times10^{-23}\ \mathrm{m\,kg\,s^{-2}\,K^{-1}}
Universal gas constant (R)8.31 J K−1 mol−18.31\ \mathrm{J\,K^{-1}\,mol^{-1}}
Stefan–Boltzmann constant (σ)5.6704×10−8 kg s−3 K−45.6704\times10^{-8}\ \mathrm{kg\,s^{-3}\,K^{-4}}
Planck constant (h)6.6261×10−34 J s6.6261\times10^{-34}\ \mathrm{J\,s}
Wien's constant (b)2.8978×10−3 m K2.8978\times10^{-3}\ \mathrm{m\,K}
Hubble constant (H₀)70 km s−1 Mpc−170\ \mathrm{km\,s^{-1}\,Mpc^{-1}}
Astronomical and Physical Constants — continuation
ConstantValue
electron charge (e)1.602×10−19 C1.602\times10^{-19}\ \mathrm C
Mass of hydrogen atom1.67×10−27 kg1.67\times10^{-27}\ \mathrm{kg}
Current inclination of the ecliptic (ε)23º 26.3′
Coordinates of the northern ecliptic pole for epoch 2000.0 (αE, δE)18h 00m 00s,+66∘ 33.6′18^{\mathrm h}\ 00^{\mathrm m}\ 00^{\mathrm s},+66^{\circ}\ 33.6^{\prime}
Coordinates of the northern galactic pole for epoch 2000.0 (αG, δG)12h 51m,+27∘ 08′12^{\mathrm h}\ 51^{\mathrm m},+27^{\circ}\ 08^{\prime}

You can try to solve an equation x=f(x)x=f(x) using iteration: xn+1=f(xn)x_{n+1}=f(x_n).

Basic equations of spherical trigonometry

sin⁡asin⁡B=sin⁡bsin⁡A\sin a\sin B=\sin b\sin A
sin⁡acos⁡B=cos⁡bsin⁡c−sin⁡bcos⁡ccos⁡A,\sin a\cos B=\cos b\sin c-\sin b\cos c\cos A,
cos⁡a=cos⁡bcos⁡c+sin⁡bsin⁡ccos⁡A.\cos a=\cos b\cos c+\sin b\sin c\cos A.

Rayleigh-Jeans formula (long wavelength approximation of Planck’s Law):

Bν(T)=2kTν2c2B_\nu(T)=\frac{2kT\nu^2}{c^2}

Условие

A moon is orbiting a planet such that the plane of its orbit is perpendicular to the surface of the planet where an observer is standing. After some necessary scaling, suppose the orbit satisfies the following equation:

9(x2+3y2−4)2+25(−3x2+y2)2=2259\left(\frac{x}{2} + \frac{\sqrt{3}y}{2} - 4\right)^2 + 25\left(-\frac{\sqrt{3}x}{2} + \frac{y}{2}\right)^2 = 225

Consider Cartesian coordinates where x is on the horizontal plane and y is on the zenith of the observer. Let rr be the radius of the moon. Assume that the period of rotation of the planet is much larger than the orbital period of the moon. Ignore the atmospheric refraction.

Tilted ellipse (the moon's orbit) drawn in x-y axes with the observer at the origin; a small circle of radius r (the moon) sits on the upper right of the ellipse, joined to the origin by a line making angle θ with the x axis.
Figure 1

a. Calculate the semimajor and semiminor axis of the ellipse.

b. Calculate the zenith angle of perigee.

c. Determine tan⁡θ2\tan\frac{\theta}{2} where θ\theta is the elevation angle (altitude of the upper tangent of the moon) when the moon looks largest to the observer.

Решение


Оригинал в Архива: Long_problem_Final_EN.pdf · официални решения: Long Problem Solution-Marking Scheme [Revised] - 310715 - 13.58.pdf · допълнителни данни: long_sol_1.png · допълнителни данни: long_sol_2.png · допълнителни данни: long_sol_3.png · допълнителни данни: long_sol_4.png · допълнителни данни: long_sol_5.png · допълнителни данни: long_sol_6.png · допълнителни данни: long_sol_7.png · допълнителни данни: long_sol_8.png · допълнителни данни: long_sol_9.png · допълнителни данни: long_sol_10.png · допълнителни данни: 9th IOAA Constants Table 20150729.pdf · допълнителни данни: constants.pdf · допълнителни данни: instructions.docx