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Solar eclipse of February 4, 1943

Total eclipse From Wikipedia, the free encyclopedia

Solar eclipse of February 4, 1943
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A total solar eclipse occurred at the Moon's descending node of orbit between Thursday, February 4 and Friday, February 5, 1943,[1] with a magnitude of 1.0331. 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 22 hours after perigee (on February 4, 1943, at 1:30 UTC), the Moon's apparent diameter was larger.[2]

Quick facts Gamma, Magnitude ...

It began on the morning on February 5 (Friday) over northeastern China (then occupied by Manchukuo), Primorsky Krai in the Soviet Union (now Russia), Hokkaido and southern Kunashir Island in Japan (Kunashir now belonging to Russia) and ended at sunset on February 4 (Thursday) over Alaska and Yukon in Canada. A partial eclipse was visible for parts of East Asia, Hawaii, and western North America.

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Observations

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In China, the eclipse occurred on February 5, the exact date of the Lunar New Year. However it was during the Second Sino-Japanese War and all the areas within the path of totality which is now in China were then under the control of Manchukuo, a Japanese puppet state. Chinese scientists did not make any observation for scientific purposes. A short report with the title "Tokyo total solar eclipse" was published in Kuomintang's official newspaper Central Daily News. Actually, Tokyo was out of the path of totality and only a partial eclipse was visible.[3]

The Japanese headquarters of the International Latitude Observatory, the predecessor of the Mizusawa VLBI Observatory [ja] of the National Astronomical Observatory of Japan in Mizusawa, Iwate (now part of the city of Ōshū) sent an observation team to Kushiro, Hokkaido. Seiichi Oikawa, a member of the team, took photos of the total eclipse.[4] In Kushiro the weather conditions were good and the solar eclipse began at 6:46 am, 11 minutes after sunrise. About 1 hour and 5 minutes later, the sun was completely covered by the moon and the totality phase was seen for less than 2 minutes.[5]

In the Territory of Alaska (now the state of Alaska), a total eclipse was visible from cities including Seward, Valdez and Kodiac. Alaska's largest city, Anchorage was located near the northern edge of the path of totality. A total eclipse was visible in the southeastern part of the city. The University of Alaska held a conference on February 4, the exact day of the eclipse, to explain in-depth information on the eclipse.[6]

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Eclipse details

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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.[7]

More information Event, Time (UTC) ...
More information Parameter, Value ...
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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.

More information February 4 Descending node (new moon), February 20 Ascending node (full moon) ...

Eclipses in 1943

Metonic

Tzolkinex

Half-Saros

Tritos

Solar Saros 120

Inex

Triad

Solar eclipses of 1942–1946

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.[8]

The partial solar eclipses on March 16, 1942 and September 10, 1942 occur in the previous lunar year eclipse set, and the partial solar eclipses on May 30, 1946 and November 23, 1946 occur in the next lunar year eclipse set.

More information series sets from 1942 to 1946, Ascending node ...

Saros 120

This eclipse is a part of Saros series 120, repeating every 18 years, 11 days, and containing 71 events. The series started with a partial solar eclipse on May 27, 933 AD. It contains annular eclipses from August 11, 1059 through April 26, 1492; hybrid eclipses from May 8, 1510 through June 8, 1564; and total eclipses from June 20, 1582 through March 30, 2033. The series ends at member 71 as a partial eclipse on July 7, 2195. 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 annularity was produced by member 11 at 6 minutes, 24 seconds on September 11, 1113, and the longest duration of totality was produced by member 60 at 2 minutes, 50 seconds on March 9, 1997. All eclipses in this series occur at the Moon’s descending node of orbit.[9]

More information Series members 50–71 occur between 1801 and 2195: ...

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.

More information 22 eclipse events between September 12, 1931 and July 1, 2011, September 11–12 ...

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.

More information Series members between 1801 and 2200 ...

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.

More information Series members between 1801 and 2200 ...
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Notes

References

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