Internet Project
Simultaneously Photographing of the Moon
and Determining its Distance
Solutions
The moon's proper motion (Example: December 9th, 2000, 21.00-21.45 UT, Tenerife)
Determination of the moon's topocentric positions for Tenerife yields the following results:
| Time | Right ascension | declination |
| 21.00 UT | 3h47m37.626s | 15°34'53".836 |
| 21.45 UT | 3h49m10.664s | 15°45'26".560 |
| Δ | 24'45".220=0.41256° |
From this result, you can derive the moon's proper motion to be 0.55008°/h. That means that it takes Tsid = 27d6h27min for a complete revolution of 360°!
Example: The moon's distance on December 9th, 2000, 21.00 UT
- The equatorial positions of Jupiter and Saturn:
- In an astronomical almanach for amateurs, you may find:
|
date | right ascension | declination |
| Jupiter | December 5th | 4h14min | 20.3° |
| December 10th | 4h11min | 20.2 |
| December 9th (calc.) | 4h11min | 20.2 |
| Saturn | November 30th | 3h40min | 17.2 |
| December 15th | 3h35min | 16.9 |
| December 9th (calc.) | 3h37min | 17.0° |
You can find the calculated values by linear interpolation.
- With an astronomical computer program you can find the following values:
| right ascension | declination |
| Jupiter | 4h11min 4.7s | 62.770° | 20°10'51" | 20.181° |
| Saturn |
3h36min28.7s |
54.120° |
17°00'55" |
17.017° |
- Determination of the angular distance between Jupiter and Saturn
- For the use of Pythagoras' theorem, you have to take into account the spherical kind of the coordinates by multiplying the right ascension alpha by the cosine of the declination delta.
The angular distance d can therefore be calculated by
d2 = (alpha*cos(delta))2 + delta2.
By this way, you will get the following result:
dJupiter, Saturn = 8.86°
-
Using spherical trigonometry, you have to use the "theorem for the cosines of sides" ("Seitencosinussatz", in German, I don't know the English terminus!):
| cos(d) |
= |
cos(90°-deltaJ)*cos(90°-deltaS)+ |
| |
sin(90°-deltaJ)*sin(90°-deltaS)* cos(alphaJ-alphaS) |
| = |
sin(deltaJ)*sin(deltaS)+ |
| |
cos(deltaJ)*cos(deltaS)*cos(alphaJ-alphaS) |
Using this formula, you will get the following result:
dJupiter, Saturn = 8.79°,
i.e., with an accuracy of about one percent, the same result as above!
- Scaling the pictures (Example: Koblenz and Namib Desert)
k.jpg) |
k.jpg) |
| Koblenz | Namib Desert |
- With an arbitrary graphic program, you can determine the pixel coordinates of Jupiter, Saturn and the moon:
| | |
x |
y |
d (J - S) |
| Koblenz |
Jupiter |
263 |
272 |
342,18
|
| |
Saturn |
605 |
261 |
| |
moon |
540 |
166 | |
| Namib Desert |
Jupiter |
507 |
226 |
416,83 |
| |
Saturn |
92 |
265 |
| |
moon |
186 |
320 | |
Therefore, the scales of the pictures are:
| Koblenz |
0,0257 o/Pixel |
| Namib Desert |
0,0211 o/Pixel |
-
With the scales known, the angular distances between the moon and either planets follow immediately from the above pixel coordinates:
| |
d (m - J) |
d (m - S) |
| |
pixels |
degrees |
pixels |
degrees |
| Koblenz |
296,59 |
7,62 |
115,11 |
2,96 |
| Namib Desert |
334,48 |
7,06 |
108,91 |
2,30 |
- Determination of the moon's parallactic displacement:
- With ruler and compasses: You can draw the either triangles into the same drawing scaled to 1°/cm, for instance.
- This construction can be replaced by combinating the both pictures:
- By measuring the distance of the either positions of the moon one gets the following result:
The moon's parallactic displacement due to Koblenz and Namib Desert is Π=1,2°
- The distance between the observers:
- On the large 21.00 UT picture of the earth Koblenz and Windhoek have the following pixel coordinates:
| x | y | d |
| Koblenz | 322 | 165 | 459 |
| Windhoek | 351 | 623 |
Because of the earth´s diameter of 768 pixels the distance, therefore, is
Δ(Koblenz, Namib Desert) = 1.195 RE = 7622 km
This value means the projection of the distance as seen by the moon.
- Our globe has a perimeter of 105.5 cm. For the length of the piece of string connecting Koblenz and Windhoek we meassured 21.8 cm. The angular distance between the either locations is, therefore:
delta = 360°*21.8/105.5 = 74.4°.
The straight line connecting them, therefore, has the length
d = 2 RE sin (delta/ 2) = 1.209RE=7712 km
- The geographical coordinates are
|
latitude |
longitude |
| Koblenz | 50°11'02" N | 07°32'16" E |
| Namib Desert | 22°28'43" S | 14°56'59" E |
With the formula given in 2. b. we get the following angular distance:
delta = 73.0°.
Therefore, the straight distance is
d = 1.190 RE = 7588 km.
- Only the result Δ in a. takes into account that the connection line between Koblenz and Namib Desert is not perpendicular to the line from the earth's center to the moon.
- The moon's distance
With the known values of Δ and the corresponding parallactic displacement Π, the distance rM to the moon can easily be determined:
- A quite good approximation results from sin(Π/2)=(Δ/2)/rM:
rM=(Δ/2)/sin(Π/2)=363800 km.
-
An even better can be derived by taking into account that the line Koblenz-Namib Desert doesn't meet the earth's center. By adding the square root of RE2+(Δ/2)2 we get, finally the following result:
rM=368900 km = 57.8 RE
- If we took into account the angle between the lines moon - earth's center and observer 1 - observer 2 we would get an even better result.
- An astronomical computer program tells us that the correct distance at the considered moment is rM = 57.74 RE!
Some more results
The following tabular shows the best results which could be derived by evaluating the pictures of the different project days:
| Date | Combination | rM | correct value |
| December, 9th, 21.00 UT | Koblenz - Namib Desert | 57.8 rE | 57.7 rE |
| Koblenz - Tenerife | 57.2 rE |
| Smolyan - Tenerife | 55.6 rE |
| Smolyan - Namib Desert | 57.4 rE |
| Tenerife - Namib Desert | 60.0 rE |
| December, 9th, 21.15 UT | Osnabrück - Tenerife | 59.1 rE |
| Osnabrück - Windhoek | 58.7 rE |
| Tenerife - Windhoek | 59.3 rE |
| January, 6th, 21.00 UT | Süderdeich - Windhoek | 58.5 rE | 57.8 rE |
| March, 1rst, 20.00 UT | Koblenz - Namib Desert | 63.8 rE | 60.1 rE |
The results would be worth to be controlled by another project participant!
Conclusions
- It is possible to "see" the moon's proper motion with a time intervall of about one hour.
- For determining the angular velocity of the moon satisfyingly, the time interval of one hour is too short.
- The moon is not infinitely far away. Simultaneously taken photos visualize the moon's parallactic shift - the more evidently the larger the distance between the observers.
- It is possible to determine the distance to the moon quite precisely. But it has become evident that for this goal
- the photos should be exposured as correctly as possible,
- the moon and the reference objects should be pictured as large scaled as possible,
- the demand of perfectness reduces with increasing distance between the observers.
- Some of our pictures were too small scaled and/or too long exposured (or the weather has been too bad!) to yield satisfying results for the distance to the moon.
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last update: June 22nd, 2008