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Solar eclipse of October 10, 1912
Total eclipse From Wikipedia, the free encyclopedia
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A total solar eclipse occurred at the Moon's descending node of orbit on Thursday, October 10, 1912,[1][2][3][4] with a magnitude of 1.0229. A solar eclipse occurs when the Moon passes between Earth and the Sun, thereby totally or partly obscuring the image of the Sun for a viewer on Earth. A total solar eclipse occurs when the Moon's apparent diameter is larger than the Sun's, blocking all direct sunlight, turning day into darkness. Totality occurs in a narrow path across Earth's surface, with the partial solar eclipse visible over a surrounding region thousands of kilometres wide. Occurring about 2.8 days after perigee (on October 7, 1912, at 18:50 UTC), the Moon's apparent diameter was larger.[5]
Totality was visible from Ecuador, Colombia, northern tip of Peru and Brazil. A partial eclipse was visible for parts of Central America, the Caribbean, South America, Antarctica, and Southern Africa.
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Observation
German physicist, mathematician and astronomer Johann Georg von Soldner calculated the gravitational lens effect in an article published in 1801. Albert Einstein got similar values in 1911, and proposed verifying it by observing the stars around the sun. The only feasible way at that time was observing during a total solar eclipse, when the sun is totally blocked. This was the first total solar eclipse after that.[6] Local teams from Brazil and international teams from the United Kingdom, France, the German Empire, Argentina and Chile made attempts in Brazil. However, it rained throughout almost the whole path of totality, and all teams failed.[7]
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Eclipse details
Summarize
Perspective
Shown below are two tables displaying details about this particular solar eclipse. The first table outlines times at which the Moon's penumbra or umbra attains the specific parameter, and the second table describes various other parameters pertaining to this eclipse.[8]
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Eclipse season
This eclipse is part of an eclipse season, a period, roughly every six months, when eclipses occur. Only two (or occasionally three) eclipse seasons occur each year, and each season lasts about 35 days and repeats just short of six months (173 days) later; thus two full eclipse seasons always occur each year. Either two or three eclipses happen each eclipse season. In the sequence below, each eclipse is separated by a fortnight.
Related eclipses
Eclipses in 1912
- A partial lunar eclipse on April 1.
- A hybrid solar eclipse on April 17.
- A partial lunar eclipse on September 26.
- A total solar eclipse on October 10.
Metonic
- Preceded by: Solar eclipse of December 23, 1908
- Followed by: Solar eclipse of July 30, 1916
Tzolkinex
- Preceded by: Solar eclipse of August 30, 1905
- Followed by: Solar eclipse of November 22, 1919
Half-Saros
- Preceded by: Lunar eclipse of October 6, 1903
- Followed by: Lunar eclipse of October 16, 1921
Tritos
- Preceded by: Solar eclipse of November 11, 1901
- Followed by: Solar eclipse of September 10, 1923
Solar Saros 142
- Preceded by: Solar eclipse of September 29, 1894
- Followed by: Solar eclipse of October 21, 1930
Inex
- Preceded by: Solar eclipse of October 30, 1883
- Followed by: Solar eclipse of September 21, 1941
Triad
- Preceded by: Solar eclipse of December 9, 1825
- Followed by: Solar eclipse of August 11, 1999
Solar eclipses of 1910–1913
This eclipse is a member of a semester series. An eclipse in a semester series of solar eclipses repeats approximately every 177 days and 4 hours (a semester) at alternating nodes of the Moon's orbit.[9]
The partial solar eclipse on August 31, 1913 occurs in the next lunar year eclipse set.
Saros 142
This eclipse is a part of Saros series 142, repeating every 18 years, 11 days, and containing 72 events. The series started with a partial solar eclipse on April 17, 1624. It contains a hybrid eclipse on July 14, 1768, and total eclipses from July 25, 1786 through October 29, 2543. There are no annular eclipses in this set. The series ends at member 72 as a partial eclipse on June 5, 2904. Its eclipses are tabulated in three columns; every third eclipse in the same column is one exeligmos apart, so they all cast shadows over approximately the same parts of the Earth.
The longest duration of totality will be produced by member 38 at 6 minutes, 34 seconds on May 28, 2291. All eclipses in this series occur at the Moon’s descending node of orbit.[10]
Metonic series
The metonic series repeats eclipses every 19 years (6939.69 days), lasting about 5 cycles. Eclipses occur in nearly the same calendar date. In addition, the octon subseries repeats 1/5 of that or every 3.8 years (1387.94 days). All eclipses in this table occur at the Moon's descending node.
Tritos series
This eclipse is a part of a tritos cycle, repeating at alternating nodes every 135 synodic months (≈ 3986.63 days, or 11 years minus 1 month). Their appearance and longitude are irregular due to a lack of synchronization with the anomalistic month (period of perigee), but groupings of 3 tritos cycles (≈ 33 years minus 3 months) come close (≈ 434.044 anomalistic months), so eclipses are similar in these groupings.
Inex series
This eclipse is a part of the long period inex cycle, repeating at alternating nodes, every 358 synodic months (≈ 10,571.95 days, or 29 years minus 20 days). Their appearance and longitude are irregular due to a lack of synchronization with the anomalistic month (period of perigee). However, groupings of 3 inex cycles (≈ 87 years minus 2 months) comes close (≈ 1,151.02 anomalistic months), so eclipses are similar in these groupings.
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Notes
Additional reading
References
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