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Astron. Astrophys. 332, 1082-1086 (1998)
3. Inter-cycle variations of facular emission
Following Foukal & Lean (1990) we assume that the shorter-term
variations of facular brightness (i.e. variations on time scales of
days to years) are well described by . This is a
reasonable choice for irradiance reconstructions aiming to cover long
periods, since only of the other proxies is
known to reproduce direct irradiance observations better, but
possesses too short a record.
We search here for possible departures from the sunspot number
record on time scales longer than a solar cycle by looking for common
features in the other four proxies. This may help us to construct a
more robust proxy from their combination. Hence we need to consider
only the ratio of the cycle-averaged value of one of the other four
proxies (let us generically call it ) to the
cycle-averaged value of :
![[EQUATION]](img15.gif)
The sum over i runs over all (or alternatively a part of)
the points in a cycle, and n is the number of the cycle
(n lies between 12 and 22).
For better comparison all values are normalized to the mean of the
cycles that are common to all five proxies, namely 18-20, i.e. we
introduce the normalized values :
![[EQUATION]](img17.gif)
We have found that the results depend only insignificantly on the
details of the normalization.
By changing the summation boundaries in Eq. (1), we are able
to estimate the contribution from different parts of a cycle. Hence,
we restrict the summation boundaries in Eq. (1) to values of
lying between two fixed boundaries, e.g. between
0-200, 0-400, 50-400 and 100-400 (cf. Paper I) and calculate an
average over the four values for each cycle. The resulting ratios
are presented in Fig. 3, where
or 10.7. Note that the summation index i
is ordered according to increasing , so that
changing the summation boundaries is equivalent to summing over
different horizontal intervals in Fig. 2. The results depend on
the summation interval most strongly for and
, due to their non-linear dependence on
. This is reflected in the larger error bars for
and in Fig. 3 which
mark the standard deviations of obtained by
varying the summation boundaries. The inter-cycle variations of
and are identical to
those already seen in Paper I. The influence of restricting the
summation over can also be judged from
Fig. 5 of that paper.
![[FIGURE]](img24.gif) |
Fig. 3. Inter-cycle variations of ratios of sunspot areas ( , solid line), 10.7cm radio flux measurements ( , dash dotted), white light facular areas ( , dashed) and Ca II K-line plage areas ( , dotted) to sunspot number. The ratios are normalized and averaged as described in the text.
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On the whole, the ratios are constant to within 20%, except for
. Whereas ,
and in Fig. 3
exhibit approximately the same level of variation, the
show a factor of four larger fluctuations.
Another striking feature is that all three proxies extending
sufficiently far back, i.e. sunspot, facular and plage areas, show a
prominent increase relative to for cycle 16. The
Ca II plage areas show an even stronger peak at cycle 19 which,
however, is absent in the other proxies, as has already been pointed
out by Foukal (1996). The peak of at cycle 16
is the only feature that is common to all data sets.
© European Southern Observatory (ESO) 1998
Online publication: March 30, 1998
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