## 3. Inter-cycle variations of facular emissionFollowing 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 : The sum over 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 : 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
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 |