The following HTML text is provided to enhance online
readability. Many aspects of typography translate only awkwardly to HTML.
Please use the page image
as the authoritative form to ensure accuracy.
Page 40
longer-term irradiance variations superimposed on the 11-year
activity cycle, such as the speculated long term increase in
irradiance from the Maunder Minimum to the present Modern
Maximum.
Lacking a detailed modeling capability for, and adequate
knowledge of, solar processes on which to base predictions,
researchers have utilized spectral analysis to develop predictive
tools. Phenomena such as sunspot numbers have periodicities on the
order of 100, 55, and 11 years, along with the solar magnetic cycle
of 22 years (e.g., Berger et al., 1990). Ice core records as well
as other climatic data suggest periods of about 80 and 180 years
(Johnsen et al., 1970), possibly related to solar activity (Otaola
and Zenteno, 1983). Extrapolation into the future of two cycles
evident in the 14 C record, at 208
years (the Suess cycle) and 88 years (the Gleissberg cycle),
suggests that the increasing solar activity that has followed the
Maunder Minimum may continue into the early twenty-first century
(Damon and Sonett, 1991), with a decline commencing around 2040.
But extrapolation of these cycles into the future and prediction of
solar effects is a highly questionable procedure, given our lack of
knowledge of the fundamental processes involved (see Chapter
6).
Wigley and Kelly (1990) have attempted to assess limits on the
role that solar forcing of climate change may play, relative to
that of greenhouse gases, during the next 200 years. Analogous to
their approach, and consistent with their results, the predictions
shown in Figure 2.5 indicate that were the Sun to experience a
period of inactivity such as the Maunder Minimum, commencing in the
year 2000, and accompanied by reduction in its radiative output of
0.25 percent, the resultant climate forcing would indeed modulate,
but not counter, the predicted anthropogenic climate forcing. As
noted previously, determining the actual climate impact of the
forcings shown in Figure 2.5 (and Figure 2.2) is difficult because
of the specific nature expected for the climate system's response
to each of the individual forcings.
Solar Activity Cycles and the
Weather
There have been many studies of the possible relationships
between weather phenomena and the 11-year solar sunspot cycle or
the 22-year solar magnetic cycle. Summaries of the results of these
studies prior to the early 1980s have been published by Herman and
Goldberg (1978) and NAS