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4. Discussion

In Table 3 (click here), we show the several equator corrections obtained from observations at Valinhos based on different selections of observational material. It seems that the better correction is that from our global reduction method.

It must be pointed out that, in our case, we estimated the equator correction and tex2html_wrap_inline1562 corrections for the declination zone of the astrolabe observations at Valinhos (tex2html_wrap_inline1986, south hemisphere) shown in Fig. 2 (click here).

  figure696
Figure 2: The declination distribution of the data

We compare the absolute declinations obtained in this paper with the published (FK5-FK4) differences. There is a good correlation between these data (Fig. 3 (click here)).

  figure702
Figure 3: Comparison of tex2html_wrap_inline1988 with tex2html_wrap_inline1990

   

Object M.E.O. tex2html_wrap_inline1560(tex2html_wrap_inline1486) tex2html_wrap_inline1996(tex2html_wrap_inline1486)remarks
Sun 1980.9 +0.07 0.14Leister (1989) - (OAM astrolabe data)
Sun1983.0 -0.01 0.04 Penna et al. (1996) - (OAM/CERGA/ON astrolabe data)
Stars 1983.0 +0.06 0.09 Clauzet et al. (1990) - (OAM astrolabe data)
Sun 1990.0 +0.08 0.07 Poppe (1994) - (OAM/CERGA astrolabe data)
Sun 1990.7 -0.03 0.01 Poppe et al. (1996) - (OAM/CERGA astrolabe data)
This paper1980.7 -0.04 0.02 Krejnin's Method
(Stars) -0.04 0.02 Krejnin's Method
+0.06 0.17 Krejnin's Method
+0.07 0.17 Krejnin's Method
-0.06 0.04 Method of Differences
+0.02 0.12 Method of Differences
+0.028 0.034 Global Reduction

Table 3: Equator corrections

The analysis of Fig. 3 (click here) confirms that the results are in agreement with the published values and that the Valinhos catalogues can represent corrections to the FK4 catalogue in the same sense that the FK5 does.


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