Understanding > Astronomical calculations
The eclipse is visible from the glacial Arctic Ocean, the north of Canada, Siberia and Greenland.
Ephemeris used to calculate positions of the Sun and Earth are the ephemeris Newcomb/ILE. For this calculation the value of TE-TU was exceptionally forced at 68.0 sec.
Julian day : : 2455714.390265
Characteristics | Values |
---|---|
Right ascension of the Sun : | 4h 37m 53.4s. |
Declination of the Sun : | +22° 05' 47.4". |
Right ascension of the Moon : | 4h 37m 41.0s. |
Declination of the Moon : | +23° 13' 19.0". |
Equatorial parallax of the Sun : | 8.7". |
Equatorial parallax of the Moon : | 55' 52.1". |
True semi-diameter of the Sun : | 15' 46.3". |
True semi-diameter of the Moon : | 15' 13.4". |
Magnitude : 0.6013
Circumstances | UT |
---|---|
Beginning of the general eclipse | the 1 at 19h 25m 17.2s |
Maximum of the eclipse | the 1 at 21h 16m 11.2s |
End of the general eclipse | the 1 at 23h 6m 57.3s |