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Solar eclipse of January 15, 2010

21st-century annular solar eclipse From Wikipedia, the free encyclopedia

Solar eclipse of January 15, 2010
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An annular solar eclipse occurred at the Moon's ascending node of orbit on Friday, January 15, 2010,[1][2][3] with a magnitude of 0.919. 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. Occurring about 1.75 days before apogee (on January 17, 2010, at 1:40 UTC), the Moon's apparent diameter was smaller.[4]

Quick Facts Gamma, Magnitude ...
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This was the longest annular solar eclipse of the millennium,[5] and the longest until December 23, 3043, with the length of maximum eclipse of 11 minutes, 7.8 seconds, and the longest duration of 11 minutes, 10.7 seconds.[6] This is about 4 minutes longer than total solar eclipses could ever get. (The solar eclipse of January 4, 1992, was longer, at 11 minutes, 40.9 seconds, occurring in the middle of the Pacific Ocean.)[7]

It was seen as an annular eclipse within a narrow stretch of 300 km (190 mi) width across the Central African Republic, the Democratic Republic of the Congo, Uganda, the Maldives, South Kerala (India), South Tamil Nadu (India), Sri Lanka and parts of Bangladesh, Burma and China. The eclipse was visible as only a partial eclipse in much of Africa, Southeastern Europe, the Middle East and Asia.

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Visibility of the eclipse

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Thumb
The eclipse in Bangui, Central African Republic at sunrise

The eclipse started in the Central African Republic near the border with Chad, traversed DR Congo, Uganda, Kenya, passed through the northern tip of Tanzania, southwestern Somalia and three islands of Seychelles (Bird, Denis and Aride), before it entered the Indian Ocean, where it reached its greatest visibility. It then passed through Maldives. The annular eclipse at Malé, the capital city of the country, started at 12:20:17 and ended at 12:31:02 local time (UTC+5), lasting for 10 minutes and 45 seconds (645 seconds). This was also the longest duration of any eclipse with an international airport in its track.[8]

At approximately 13:20 IST, the annular solar eclipse entered India at Thiruvananthapuram (Trivandrum), the capital of Kerala and exited India at Rameswaram, Tamil Nadu.

The eclipse was viewable for 10 minutes in India. After Rameswaram, it entered Sri Lanka at Delft Island, exited at Jaffna in Sri Lanka, crossed the Bay of Bengal and re-entered India in Mizoram.

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The eclipse from Thiruvananthapuram, India where the eclipse was 92%

Thiruvananthapuram, which was the entry point of the eclipse in India, was equipped with telescopes and announced facilities for the public to view the eclipse.[9] Vikram Sarabhai Space Centre, situated in Trivandrum, analysed the atmospheric-ionospheric parameters during the eclipse.[10] Many scientists camped in the city to witness and study the eclipse.[11]

At Rameswaram, the sunrise was not visible due to thick clouds, but it started getting clear at around 9 am local time and became almost totally clear by the time the eclipse began. The sky had a thin layer of cirrus clouds till 2:30 pm. Among the eclipse-watchers was Sky Watchers' Association of North Bengal (SWAN) from Siliguri at the foothills of West Bengal and Tamil Nadu Astronomical Association.

Dhanushkodi, which falls on the central line of the eclipse, was a good place to view the eclipse. The northernmost limit of shadow in India was Cuddalore, Neyveli, Erode, Kodaikanal, and Madurai. Other prime viewing locations in Tamil Nadu include Thoothukudi and Cape Comorin, 22 km north of the center line. The exact location of the line is between the NH end and the Dhanushkodi ruins. Dhanushkodi is about 2 km east of the central line. The degree difference is about 0.2 between the central line – with Kodandaramar Temple and Dhanushkodi ruins vice versa. Dhanushkodi is about 5 km from the Kodandaramar Temple.

After South Asia, the antumbra passed through the southern tip of Bangladesh, Myanmar and China before leaving the Earth.

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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.[12]

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

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 December 31Descending node (full moon), January 15Ascending node (new moon) ...
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Eclipses in 2010

Metonic

Tzolkinex

Half-Saros

Tritos

Solar Saros 141

Inex

Triad

Solar eclipses of 2008–2011

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.[13]

The partial solar eclipses on June 1, 2011 and November 25, 2011 occur in the next lunar year eclipse set.

More information series sets from 2008 to 2011, Ascending node ...

Saros 141

This eclipse is a part of Saros series 141, repeating every 18 years, 11 days, and containing 70 events. The series started with a partial solar eclipse on May 19, 1613. It contains annular eclipses from August 4, 1739 through October 14, 2640. There are no hybrid or total eclipses in this set. The series ends at member 70 as a partial eclipse on June 13, 2857. 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 20 at 12 minutes, 9 seconds on December 14, 1955. All eclipses in this series occur at the Moon’s ascending node of orbit.[14]

More information Series members 12–33 occur between 1801 and 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.

More information 20 eclipse events between June 10, 1964 and August 21, 2036, June 10–11 ...

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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