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Next: Field shifts Up: No Title Previous: Special cases of the SYN projection: SIN and

Correction for precession

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 ($ \alpha_{p}^{}$,$ \delta_{p}^{}$) are the J2000.0 right ascension and declination of the apparent pole then


nu = -cos$\displaystyle \delta_{p}^{}$sin($\displaystyle \alpha_{p}^{}$ - $\displaystyle \alpha_{0}^{}$) (15)
nv = sin$\displaystyle \delta_{p}^{}$cos$\displaystyle \delta_{0}^{}$ - cos$\displaystyle \delta_{p}^{}$sin$\displaystyle \delta_{0}^{}$cos($\displaystyle \alpha_{p}^{}$ - $\displaystyle \alpha_{0}^{}$)  
nw = sin$\displaystyle \delta_{p}^{}$sin$\displaystyle \delta_{0}^{}$ + cos$\displaystyle \delta_{p}^{}$cos$\displaystyle \delta_{0}^{}$cos($\displaystyle \alpha_{p}^{}$ - $\displaystyle \alpha_{0}^{}$)  

These may be substituted directly into equations (7) and (8). Precession from 1990 to 2000 amounts to about 3'. For $ \alpha_{p}^{}$ = $ \alpha_{0}^{}$ and $ \delta_{0}^{}$ = 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.


next up previous
Next: Field shifts Up: No Title Previous: Special cases of the SYN projection: SIN and
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2006-03-28