Solar eclipse of May 9, 1948

Solar eclipse of May 9, 1948
Map
Type of eclipse
Nature	Annular
Gamma	0.4133
Magnitude	0.9999
Maximum eclipse
Duration	0 s (0 min 0 s)
Coordinates	39°48′N131°12′E / 39.8°N 131.2°E / 39.8; 131.2
Times (UTC)
Greatest eclipse	2:26:04
References
Saros	137 (32 of 70)
Catalog # (SE5000)	9394

An annular solar eclipse occurred at the Moon's ascending node of orbit between Saturday, May 8 and Sunday, May 9, 1948, ^[1] with a magnitude of 0.9999. 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. An annular solar eclipse occurs when the Moon's apparent diameter is smaller than the Sun's, blocking most of the Sun's light and causing the Sun to look like an annulus (ring). An annular eclipse appears as a partial eclipse over a region of the Earth thousands of kilometres wide. The Moon's apparent diameter was near the average diameter because it occurred 7 days after apogee (on May 2, 1948, at 2:00 UTC) and 6.7 days before perigee (on May 15, 1948, at 17:10 UTC). ^[2]

The moon's apparent diameter was only 0.006% smaller than the Sun's, so this was an annular solar eclipse that occurred on May 9. The path width of this large annular solar eclipse, was about 200 meters and lasted only 0.3 seconds. The large annular eclipse covered over 99% of the Sun, creating a dramatic spectacle for observers in only an extremely narrow strip; however, it was fleeting, lasting just moments at the point of maximum eclipse.

Annularity was visible from Car Nicobar, the northernmost of the Nicobar Islands, and Burma, Siam (now renamed to Thailand) including Bangkok, French Indochina (the part now belonging to Laos), North Vietnam (now belonging to Vietnam), China, South Korea, Rebun Island in Japan, Kuril Islands in the Soviet Union (now belonging to Russia) on May 9, and Alaska on May 8. A partial eclipse was visible for parts of South Asia, Southeast Asia, East Asia, Northeast Asia, Alaska, and northwest Canada.

This was the first of four central solar eclipses visible from Bangkok from 1948 to 1958, where it is extremely rare for a large city to witness four central solar eclipses within 10 years.

Observations

During this eclipse, the apex of the moon's umbral cone was very close to the Earth's surface, and the magnitude was very large. The edges of the moon and the sun were very close to each other as seen from the Earth. Baily's beads on the lunar limb, which are usually only visible during a total solar eclipse, could also be seen. Therefore this eclipse was also an excellent opportunity to measure the size and shape of the Earth, as well as the mountains and valleys on the lunar limb. The National Geographic Society sent 7 teams respectively to Myeik in Burma, Bangkok in Siam, Wukang County (now belonging to Deqing County, Zhejiang) in China, Onyang-eup  [ ko ] of Asan-gun  [ ko ] (now Onyang-dong, Asan City) in South Korea, Rebun Island in Japan, Adak Island in Alaska, as well as from the air onboard a Boeing B-29 Superfortress departing from Shemya Island. The scale of this observation was larger than ever before. In the end, the teams from the air and on Rebun Island got the best results with good weather conditions, while the results in Myeik and Bangkok were relatively good, Adak Island still somewhat valuable, Onyang-eup missing many goals, and Wukang with the worst results where there was rain during the eclipse. It was shortly after the end of World War II, and the observation in Japan showed friendship among the science community. ^[3] Kafuka  [ ja ], one of the two villages on the island, supported the observation team, and a Solar Eclipse Observation Monument was built in 1954 to commemorate it. ^{[4] [5]} The monument was first erected in Kitousu, the center of the observation site. It was moved to Itsukushima Shrine in 2003, across the sea facing Rishirifuji. ^[6]

Prior to it, the two hybrid solar eclipses of April 17, 1912 and April 28, 1930, also belonging to Solar Saros 137, also occurred with a magnitude close to 1. Observations were made near Paris, France and Camptonville, California respectively. There was an opportunity to make similar observations during the annular solar eclipse of May 20, 1966 in Greece and Turkey, also belonging to the same solar Saros cycle. ^[4]

The Institute of Astronomy of the Academia Sinica (predecessor of Purple Mountain Observatory), Department of Physics of National Central University and Bureau of Surveying of the Ministry of National Defense also formed a team. The initial plan was to go to Guangdong, far from the observation site of the American team, hoping that the two teams would not be affected by bad weather at the same time. However after checking the weather, traffic and law and order conditions near Guangzhou, Hangzhou and Suzhou, the team finally decided on Cibiwu in Yuhang County. The decision was made based on the fact that meteorological data showed bad conditions generally across the whole Jiangnan in May, within the East Asian rainy season, and funding is limited so travel could not be made for a long distance. Besides, Xujiahui (Zi-Ka-Wei) Observatory estimated that there was 70% hope in Cibiwu, and it is close to the observation site of the American team, allowing the Chinese team to see the equipment of the American team for future reference. ^[7] Zhang Yuzhe, director of the Institute of Astronomy, visited the United States and Canada to study the spectrum of eclipsing binaries in 1946. However, the Ministry of Foreign Affairs of the Republic of China stopped funding him the return trip back to China. He took the opportunity of joining the observation team to return to China in March 1948, ^[8] and observed it together with Chen Zungui  [ zh ]. ^[9] In the end, due to the weather conditions, just like the American team which traveled to China, the Chinese team also only measured changes in the luminosity of the sun. The Qingdao Observatory, Sun Yat-sen University Observatory and the Department of Physics of Tongji University also made observations. ^[10]

Eclipse details

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. ^[11]

May 9, 1948 Solar Eclipse Times

Event	Time (UTC)
First Penumbral External Contact	1948 May 08 at 23:40:23.2 UTC
First Umbral External Contact	1948 May 09 at 00:44:35.7 UTC
First Central Line	1948 May 09 at 00:45:07.7 UTC
Greatest Duration	1948 May 09 at 00:45:07.7 UTC
First Umbral Internal Contact	1948 May 09 at 00:45:39.6 UTC
First Penumbral Internal Contact	1948 May 09 at 02:06:53.9 UTC
Greatest Eclipse	1948 May 09 at 02:26:03.6 UTC
Ecliptic Conjunction	1948 May 09 at 02:30:35.8 UTC
Equatorial Conjunction	1948 May 09 at 02:44:18.7 UTC
Last Penumbral Internal Contact	1948 May 09 at 02:44:48.6 UTC
Last Umbral Internal Contact	1948 May 09 at 04:06:18.3 UTC
Last Central Line	1948 May 09 at 04:06:47.3 UTC
Last Umbral External Contact	1948 May 09 at 04:07:16.3 UTC
Last Penumbral External Contact	1948 May 09 at 05:11:30.1 UTC

May 9, 1948 Solar Eclipse Parameters

Parameter	Value
Eclipse Magnitude	0.99994
Eclipse Obscuration	0.99989
Gamma	0.41332
Sun Right Ascension	03h03m37.8s
Sun Declination	+17°18'09.3"
Sun Semi-Diameter	15'50.3"
Sun Equatorial Horizontal Parallax	08.7"
Moon Right Ascension	03h03m01.1s
Moon Declination	+17°40'05.5"
Moon Semi-Diameter	15'36.6"
Moon Equatorial Horizontal Parallax	0°57'17.4"
ΔT	28.4 s

Eclipse season

See also: Eclipse cycle

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.

Eclipse season of April–May 1948

April 23 Descending node (full moon)	May 9 Ascending node (new moon)
Partial lunar eclipse Lunar Saros 111	Annular solar eclipse Solar Saros 137

Related eclipses

Eclipses in 1948

• A partial lunar eclipse on April 23.
• An annular solar eclipse on May 9.
• A penumbral lunar eclipse on October 18.
• A total solar eclipse on November 1.

Metonic

• Preceded by: Solar eclipse of July 20, 1944
• Followed by: Solar eclipse of February 25, 1952

Tzolkinex

• Preceded by: Solar eclipse of March 27, 1941
• Followed by: Solar eclipse of June 20, 1955

Half-Saros

• Preceded by: Lunar eclipse of May 3, 1939
• Followed by: Lunar eclipse of May 13, 1957

Tritos

• Preceded by: Solar eclipse of June 8, 1937
• Followed by: Solar eclipse of April 8, 1959

Solar Saros 137

• Preceded by: Solar eclipse of April 28, 1930
• Followed by: Solar eclipse of May 20, 1966

Inex

• Preceded by: Solar eclipse of May 29, 1919
• Followed by: Solar eclipse of April 18, 1977

Triad

• Preceded by: Solar eclipse of July 8, 1861
• Followed by: Solar eclipse of March 9, 2035

Solar eclipses of 1946–1949

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. ^[12]

The partial solar eclipses on January 3, 1946 and June 29, 1946 occur in the previous lunar year eclipse set.

Solar eclipse series sets from 1946 to 1949
Ascending node				Descending node
Saros	Map	Gamma		Saros	Map	Gamma
117	May 30, 1946 Partial	−1.0711		122	November 23, 1946 Partial	1.105
127	May 20, 1947 Total	−0.3528		132	November 12, 1947 Annular	0.3743
137	May 9, 1948 Annular	0.4133		142	November 1, 1948 Total	−0.3517
147	April 28, 1949 Partial	1.2068		152	October 21, 1949 Partial	−1.027

Saros 137

This eclipse is a part of Saros series 137, repeating every 18 years, 11 days, and containing 70 events. The series started with a partial solar eclipse on May 25, 1389. It contains total eclipses from August 20, 1533 through December 6, 1695; the first set of hybrid eclipses from December 17, 1713 through February 11, 1804; the first set of annular eclipses from February 21, 1822 through March 25, 1876; the second set of hybrid eclipses from April 6, 1894 through April 28, 1930; and the second set of annular eclipses from May 9, 1948 through April 13, 2507. The series ends at member 70 as a partial eclipse on June 28, 2633. 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 was produced by member 11 at 2 minutes, 55 seconds on September 10, 1569, and the longest duration of annularity will be produced by member 59 at 7 minutes, 5 seconds on February 28, 2435. All eclipses in this series occur at the Moon’s ascending node of orbit. ^[13]

Series members 24–46 occur between 1801 and 2200:
24	25	26
February 11, 1804	February 21, 1822	March 4, 1840
27	28	29
March 15, 1858	March 25, 1876	April 6, 1894
30	31	32
April 17, 1912	April 28, 1930	May 9, 1948
33	34	35
May 20, 1966	May 30, 1984	June 10, 2002
36	37	38
June 21, 2020	July 2, 2038	July 12, 2056
39	40	41
July 24, 2074	August 3, 2092	August 15, 2110
42	43	44
August 25, 2128	September 6, 2146	September 16, 2164
45	46
September 27, 2182	October 9, 2200

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 ascending node.

22 eclipse events between December 13, 1898 and July 20, 1982
December 13–14	October 1–2	July 20–21	May 9	February 24–25
111	113	115	117	119
December 13, 1898		July 21, 1906	May 9, 1910	February 25, 1914
121	123	125	127	129
December 14, 1917	October 1, 1921	July 20, 1925	May 9, 1929	February 24, 1933
131	133	135	137	139
December 13, 1936	October 1, 1940	July 20, 1944	May 9, 1948	February 25, 1952
141	143	145	147	149
December 14, 1955	October 2, 1959	July 20, 1963	May 9, 1967	February 25, 1971
151	153	155
December 13, 1974	October 2, 1978	July 20, 1982

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.

Series members between 1801 and 2200
June 16, 1806 (Saros 124)	May 16, 1817 (Saros 125)	April 14, 1828 (Saros 126)	March 15, 1839 (Saros 127)	February 12, 1850 (Saros 128)
January 11, 1861 (Saros 129)	December 12, 1871 (Saros 130)	November 10, 1882 (Saros 131)	October 9, 1893 (Saros 132)	September 9, 1904 (Saros 133)
August 10, 1915 (Saros 134)	July 9, 1926 (Saros 135)	June 8, 1937 (Saros 136)	May 9, 1948 (Saros 137)	April 8, 1959 (Saros 138)
March 7, 1970 (Saros 139)	February 4, 1981 (Saros 140)	January 4, 1992 (Saros 141)	December 4, 2002 (Saros 142)	November 3, 2013 (Saros 143)
October 2, 2024 (Saros 144)	September 2, 2035 (Saros 145)	August 2, 2046 (Saros 146)	July 1, 2057 (Saros 147)	May 31, 2068 (Saros 148)
May 1, 2079 (Saros 149)	March 31, 2090 (Saros 150)	February 28, 2101 (Saros 151)	January 29, 2112 (Saros 152)	December 28, 2122 (Saros 153)
November 26, 2133 (Saros 154)	October 26, 2144 (Saros 155)	September 26, 2155 (Saros 156)	August 25, 2166 (Saros 157)	July 25, 2177 (Saros 158)
June 24, 2188 (Saros 159)	May 24, 2199 (Saros 160)

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.

Series members between 1801 and 2200
August 17, 1803 (Saros 132)	July 27, 1832 (Saros 133)	July 8, 1861 (Saros 134)
June 17, 1890 (Saros 135)	May 29, 1919 (Saros 136)	May 9, 1948 (Saros 137)
April 18, 1977 (Saros 138)	March 29, 2006 (Saros 139)	March 9, 2035 (Saros 140)
February 17, 2064 (Saros 141)	January 27, 2093 (Saros 142)	January 8, 2122 (Saros 143)
December 19, 2150 (Saros 144)	November 28, 2179 (Saros 145)

Notes

1. "May 8–9, 1948 Total Solar Eclipse". timeanddate. Retrieved 4 August 2024.
2. "Moon Distances for London, United Kingdom, England". timeanddate. Retrieved 4 August 2024.
3. Kinney, William A., Moore, W. Robert, Williams, Maynard Owen, William A. Kinney, W. Robert Moore and Maynard Owen Williams. "Operation Eclipse: 1948". National Geographic Magazine. Archived from the original on 21 August 2019.
4. Xavier M. Jubier. "Eclipse annulaire de Soleil du 9 mai 1948 depuis le Japon (Annular Solar Eclipse of 1948 May 9 in Japan)". Archived from the original on 27 August 2019.
5. "1948年5月9日 - 礼文島でたった1秒の金環日食" (in Japanese). 日食ナビ. Archived from the original on 5 March 2016.
6. "礼文島における金環日蝕観測" (in Japanese). Hokkaido Museum Association. Archived from the original on 25 October 2020.
7. Chen Zungui (1948). "餘杭觀測日食經過". 宇宙 (in Chinese): 84–85.
8. "张钰哲" (in Chinese). 闽都文化研究会. Archived from the original on 31 August 2019.
9. "大事记（1912-1982）" (in Chinese). Chinese Astronomical Society. Archived from the original on 15 May 2020.
10. Bai Shouyi. "《中国通史》第十二卷 近代后编（1919－1949）（下册）·第四节 日食观测" (in Chinese). Archived from the original on 10 November 2019.
11. "Annular Solar Eclipse of 1948 May 09". EclipseWise.com. Retrieved 4 August 2024.
12. van Gent, R.H. "Solar- and Lunar-Eclipse Predictions from Antiquity to the Present". A Catalogue of Eclipse Cycles. Utrecht University. Retrieved 6 October 2018.
13. "NASA - Catalog of Solar Eclipses of Saros 137". eclipse.gsfc.nasa.gov.

References

• Earth visibility chart and eclipse statistics Eclipse Predictions by Fred Espenak, NASA/GSFC
  • Google interactive map
  • Besselian elements