As we have mentioned in Sect. 4.3, during the time covered
by the data presented here, the solar activity had probably reached its
maximum. To be more precise, since the current solar cycle (No. 23) has
a double peak structure (see Fig. 6), our measurements cover
the descent from the first maximum and the abrupt increase to the second
maximum. Mainly due to the latter transition, the solar density flux
at 10.7 cm in our data set ranges from 1.2 MJy to 2.4 MJy, the median value
being 1.8 MJy.
Even though this is almost half of the full range expected on a typical
complete 11 years solar cycle (0.8-2.5 MJy), a clear
variation is seen in the same solar density flux range from similar analysis
performed by other authors (see for example Mattila et al. 1996, their
Fig. 6). In Fig. 13 we show the case of the R passband, where
we have plotted the nightly average sky brightness vs. the solar density flux
measured during the day immediately preceeding the observations. A linear
least squares fit to the data (solid line) gives a slope of
0.14
0.01 mag arcsec-2 MJy-1, which turns
into a variation of 0.24
0.11 mag arcsec-2 during a full solar
cycle. This value is a factor two smaller than what has been reported
for B, V (Walker 1988b; Krisciunas 1990) and uvgyr
(Leinert et al. 1995; Mattila et al. 1996) for yearly averages and it is
consistent with a null variation at the 2 sigma level. Moreover,
since the correlation factor computed for the data in Fig. 13
is only 0.19, we think there is no clear indication for a real dependency.
This impression is confirmed by the fact that a similar analysis for
the B and V passbands gives an extrapolated variation of 0.08
0.13
and 0.07
0.11 mag arcsec-2 respectively. These numbers, which
are consistent with zero, and the low correlation coefficients
(0.08 and 0.11 respectively) seem to indicate no short-term dependency
from the 10.7 cm solar flux. Similar values
are found for the I passband (
0.22
0.15 mag arcsec-2).
These results agree with the findings by Leinert et al. (1995)
and Mattila et al. (1996) and the early work of
Rosenberg & Zimmermann (1967), who have shown that the [OI]5577 Å line intensity correlates with the 2800 MHz solar flux much more
strongly using the monthly averages than the nightly averages.
For all these reasons, we agree with Mattila et al. (1996) in saying
that no firm prediction on the night sky brightness can be made on the basis
of the solar flux measured during the day preceeding the observations,
as it was initially suggested by Walker (1988b).
A possible physical explanation for this effect is that there is some inertia
in the energy release from the layers ionised by the solar UV radiation, such
that what counts is the integral over some typical time scale rather than
the instantaneous energy input.
Copyright ESO 2003