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Partial eclipse | |||||||||||||
Date | July 15, 1916 | ||||||||||||
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Gamma | −0.5957 | ||||||||||||
Magnitude | 0.7944 | ||||||||||||
Saros cycle | 118 (46 of 74) | ||||||||||||
Partiality | 172 minutes, 30 seconds | ||||||||||||
Penumbral | 292 minutes, 24 seconds | ||||||||||||
| |||||||||||||
A partial lunar eclipse occurred at the Moon’s ascending node of orbit on Saturday, July 15, 1916,[1] with an umbral magnitude of 0.7944. A lunar eclipse occurs when the Moon moves into the Earth's shadow, causing the Moon to be darkened. A partial lunar eclipse occurs when one part of the Moon is in the Earth's umbra, while the other part is in the Earth's penumbra. Unlike a solar eclipse, which can only be viewed from a relatively small area of the world, a lunar eclipse may be viewed from anywhere on the night side of Earth. Occurring only about 3.5 hours after perigee (on July 15, 1916, at 1:15 UTC), the Moon's apparent diameter was larger.[2]
The Ross Sea party was a component of Sir Ernest Shackleton's Imperial Trans-Antarctic Expedition of 1914–17. Five men were stranded not far away from Cape Evans. There was sea ice between them and the relative safety of the hut on Cape Evans. On May 8 two of the men, Aeneas Mackintosh and Victor Hayward, decided to make an attempt to reach the hut. Soon after they set out, a blizzard hit. When the weather cleared up, the remaining men tried to look for them, but realized that the ice was far too thin to cross, and that their friends had been lost. Now they knew that they should wait for a thicker ice and for the full moon to attempt the crossing. Having the full moon was essential, because during polar night the moon is the only source of natural light other than the extremely dim light of the stars.
The weather did not cooperate during the full moon of June, but on July 15, everything seemed to be just right: calm weather, thick ice, clear skies and a full moon. The men started their journey in the morning. When the moon rose, however, the men were surprised to find it was about to be eclipsed[citation needed]. Ernest Wild wrote later:
"I thought we were going to be left in darkness but a very little bit of the rim remained to light us..."
Although the eclipse continued for a few hours, the men were fortunate because it was only a partial eclipse. They reached Cape Evans later on the same day.[3]
The eclipse was completely visible over eastern North America, South America, and Antarctica, seen rising over western North America and the central Pacific Ocean and setting over Africa and western Europe.[4]
Shown below is a table displaying details about this particular solar eclipse. It describes various parameters pertaining to this eclipse.[5]
Parameter | Value |
---|---|
Penumbral Magnitude | 1.73508 |
Umbral Magnitude | 0.79437 |
Gamma | −0.59568 |
Sun Right Ascension | 07h36m32.1s |
Sun Declination | +21°35'52.3" |
Sun Semi-Diameter | 15'44.1" |
Sun Equatorial Horizontal Parallax | 08.7" |
Moon Right Ascension | 19h37m12.9s |
Moon Declination | -22°11'11.4" |
Moon Semi-Diameter | 16'43.6" |
Moon Equatorial Horizontal Parallax | 1°01'23.4" |
ΔT | 18.8 s |
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.
July 15 Ascending node (full moon) |
July 30 Descending node (new moon) |
---|---|
Penumbral lunar eclipse Lunar Saros 118 |
Annular solar eclipse Solar Saros 144 |
This eclipse is a member of a semester series. An eclipse in a semester series of lunar eclipses repeats approximately every 177 days and 4 hours (a semester) at alternating nodes of the Moon's orbit.[6]
The penumbral lunar eclipses on March 1, 1915 and August 24, 1915 occur in the previous lunar year eclipse set.
Lunar eclipse series sets from 1915 to 1918 | ||||||||
---|---|---|---|---|---|---|---|---|
Descending node | Ascending node | |||||||
Saros | Date Viewing |
Type Chart |
Gamma | Saros | Date Viewing |
Type Chart |
Gamma | |
103 | 1915 Jan 31 |
Penumbral |
1.5450 | 108 | 1915 Jul 26 |
Penumbral |
−1.3553 | |
113 | 1916 Jan 20 |
Partial |
0.9146 | 118 | 1916 Jul 15 |
Partial |
−0.5956 | |
123 | 1917 Jan 08 |
Total |
0.2415 | 128 | 1917 Jul 04 |
Total |
0.1419 | |
133 | 1917 Dec 28 |
Total |
−0.4484 | 138 | 1918 Jun 24 |
Partial |
0.9397 | |
133 | 1918 Dec 17 |
Penumbral |
−1.1035 |
This eclipse is a part of Saros series 118, repeating every 18 years, 11 days, and containing 73 events. The series started with a penumbral lunar eclipse on March 2, 1105. It contains partial eclipses from June 8, 1267 through August 12, 1375; total eclipses from August 22, 1393 through June 22, 1880; and a second set of partial eclipses from July 3, 1898 through September 18, 2024. The series ends at member 73 as a penumbral eclipse on May 7, 2403.
The longest duration of totality was produced by member 37 at 99 minutes, 22 seconds on April 7, 1754. All eclipses in this series occur at the Moon’s ascending node of orbit.[7]
Greatest | First | |||
---|---|---|---|---|
The greatest eclipse of the series occurred on 1754 Apr 07, lasting 99 minutes, 22 seconds.[8] | Penumbral | Partial | Total | Central |
1105 Mar 02 |
1267 Jun 08 |
1393 Aug 22 |
1465 Oct 04 | |
Last | ||||
Central | Total | Partial | Penumbral | |
1826 May 21 |
1880 Jun 22 |
2024 Sep 18 |
2403 May 07 |
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.
Series members 40–61 occur between 1801 and 2200: | |||||
---|---|---|---|---|---|
40 | 41 | 42 | |||
1808 May 10 | 1826 May 21 | 1844 May 31 | |||
43 | 44 | 45 | |||
1862 Jun 12 | 1880 Jun 22 | 1898 Jul 03 | |||
46 | 47 | 48 | |||
1916 Jul 15 | 1934 Jul 26 | 1952 Aug 05 | |||
49 | 50 | 51 | |||
1970 Aug 17 | 1988 Aug 27 | 2006 Sep 07 | |||
52 | 53 | 54 | |||
2024 Sep 18 | 2042 Sep 29 | 2060 Oct 09 | |||
55 | 56 | 57 | |||
2078 Oct 21 | 2096 Oct 31 | 2114 Nov 12 | |||
58 | 59 | 60 | |||
2132 Nov 23 | 2150 Dec 04 | 2168 Dec 14 | |||
61 | |||||
2186 Dec 26 | |||||
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.
Series members between 1801 and 2200 | |||||||||
---|---|---|---|---|---|---|---|---|---|
1807 May 21 (Saros 108) |
1818 Apr 21 (Saros 109) |
1829 Mar 20 (Saros 110) |
1840 Feb 17 (Saros 111) |
1851 Jan 17 (Saros 112) | |||||
1861 Dec 17 (Saros 113) |
1872 Nov 15 (Saros 114) |
1883 Oct 16 (Saros 115) |
1894 Sep 15 (Saros 116) |
1905 Aug 15 (Saros 117) | |||||
1916 Jul 15 (Saros 118) |
1927 Jun 15 (Saros 119) |
1938 May 14 (Saros 120) |
1949 Apr 13 (Saros 121) |
1960 Mar 13 (Saros 122) | |||||
1971 Feb 10 (Saros 123) |
1982 Jan 09 (Saros 124) |
1992 Dec 09 (Saros 125) |
2003 Nov 09 (Saros 126) |
2014 Oct 08 (Saros 127) | |||||
2025 Sep 07 (Saros 128) |
2036 Aug 07 (Saros 129) |
2047 Jul 07 (Saros 130) |
2058 Jun 06 (Saros 131) |
2069 May 06 (Saros 132) | |||||
2080 Apr 04 (Saros 133) |
2091 Mar 05 (Saros 134) |
2102 Feb 03 (Saros 135) |
2113 Jan 02 (Saros 136) |
2123 Dec 03 (Saros 137) | |||||
2134 Nov 02 (Saros 138) |
2145 Sep 30 (Saros 139) |
2156 Aug 30 (Saros 140) |
2167 Aug 01 (Saros 141) |
2178 Jun 30 (Saros 142) | |||||
2189 May 29 (Saros 143) |
2200 Apr 30 (Saros 144) | ||||||||
A lunar eclipse will be preceded and followed by solar eclipses by 9 years and 5.5 days (a half saros).[9] This lunar eclipse is related to two annular solar eclipses of Solar Saros 125.
July 10, 1907 | July 20, 1925 |
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