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The plane of an east-west array coincides with the apparent equatorial plane
at the date of the observation and this is tilted slightly with respect to the
J2000.0 equatorial plane. If
(,
) are the J2000.0 right
ascension and declination of the apparent pole then
nu | = | -cos![]() ![]() ![]() |
(15) |
nv | = | sin![]() ![]() ![]() ![]() ![]() ![]() |
|
nw | = | sin![]() ![]() ![]() ![]() ![]() ![]() |
These may be substituted directly into equations (7) and
(8). Precession from 1990 to 2000 amounts to about 3'. For
=
and
= 30o we get
p1 | = | 0 | |
p2 | = | 1.72857 |
Equations 12 with no precession correction give
p1 | = | 0 | |
p2 | = | 1.73205 |
For a position 1o from the field centre at this declination the difference between these amounts to about 0".1.