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A 1200-Year History of Total Solar Irradiance
Volume 6, Number 36: 3 September 2003

In the introduction to their paper on solar irradiance variations over the last 1200 years, Bard et al. (2000) list some of the many different types of information that have been used to reconstruct past solar variability, including "the envelope of the SSN [sunspot number] 11-year cycle (Reid, 1991), the length and decay rate of the solar cycle (Hoyt and Schatten, 1993), the structure and decay rate of individual sunspots (Hoyt and Schatten, 1993), the mean level of SSN (Hoyt and Schatten, 1993; Zhang et al., 1994; Reid, 1997), the solar rotation and the solar diameter (Nesme-Ribes et al., 1993), and the geomagnetic aa index (Cliver et al., 1998)."  They also note that "Lean et al. (1995) proposed that the irradiance record could be divided into 2 superimposed components: an 11-year cycle based on the parameterization of sunspot darkening and facular brightening (Lean et al., 1992), and a slowly-varying background derived separately from studies of sun-like stars (Baliunas and Jastrow, 1990)," and that Solanki and Fligge (1998) have developed an even more convoluted technique.

In the case of the paper that is the subject of this Editorial (Bard et al., 2000), an entirely different approach is used.  Rather than directly characterizing some aspect of solar variability, certain consequences of that variability are assessed.  Specifically, the authors note that magnetic fields of the solar wind deflect portions of the primary flux of charged cosmic particles in the vicinity of the earth, leading to reductions in the creation of cosmogenic nuclides in earth's atmosphere.  Consequently, histories of the atmospheric concentrations of 14C and 10Be can be used as proxies for solar activity, as noted many years ago by Lal and Peters (1967).

In employing this approach to the problem, the authors first created a 1200-year history of cosmonuclide production in earth's atmosphere from 10Be measurements of South Pole ice (Raisbeck et al., 1990) and the atmospheric 14C/12C record as measured in tree rings (Bard et al., 1997).  This record was then converted to Total Solar Irradiance (TSI) values by "applying a linear scaling using the TSI values published previously for the Maunder Minimum," when cosmonuclide production was 30-50% above the modern value.

The authors' work resulted in an extended TSI record that suggests, in their words, that "solar output was significantly reduced between 1450 and 1850 AD, but slightly higher or similar to the present value during a period centered around 1200 AD."  Hence, they say "it could thus be argued that irradiance variations may have contributed to the so-called "little ice age" and "medieval warm period."

In discussing this idea, Bard et al. amazingly downplay their own suggestion, because, as they report, "some researchers have concluded that the 'little ice age' and/or 'medieval warm period' [were] regional, rather than global events."  Noting that the TSI variations they developed from their cosmonuclide data "would tend to force global effects," they felt they could not associate this global impetus for climate change with what other people were calling regional climatic anomalies.

With respect to these thoughts, we note that "some researchers" have indeed been working overtime to rewrite this aspect of earth's climatic history, claiming that both the Little Ice Age and Medieval Warm Period were restricted to lands bordering on the North Atlantic Ocean.  However, as may readily be seen by perusing the many materials we have filed under the headings of Little Ice Age and Medieval Warm Period in our Subject Index, these phenomena were truly global in extent.  Hence, when Bard et al. say their TSI variations "would tend to force global effects," they truly hit the nail on the head, as their global forcing function meshes well with the global climatic response of the earth.

Additional support for the TSI record developed by Bard et al., as well as its global climatic implications, is provided by two other studies we have reviewed.  Rigozo et al. (2001) developed a 1000-year record of sunspot number, which they say "reproduces well the great maximums and minimums in solar activity, identified in cosmonuclide variation records, and, specifically, the epochs of the Oort, Wolf, Sporer, Maunder, and Dalton Minimums, as well [as] the Medieval and Modern Maximums."  Likewise, Pang and Yau (2002) -- using similar data, but augmented by numerous Chinese, Japanese and Korean records of sunspot sightings -- developed an 1800-year history of solar brightness change that reveals these same solar minima and maxima, which include those found by Bard et al.

Truly, the evidence for the solar forcing of climate on centennial and millennial time scales, as well as both shorter and longer periods, is overwhelming.  And with each passing day, it grows ever more substantial.

Sherwood, Keith and Craig Idso

Baliunas, S. and Jastrow, R.  1990.  Evidence for long-term brightness changes of solar-type stars.  Nature 348: 520-522.

Bard, E., Raisbeck, G., Yiou, F. and Jouzel, J.  1997.  Solar modulation of cosmogenic nuclide production over the last millennium: comparison between 14C and 10Be records.  Earth and Planetary Science Letters 150: 453-462.

Bard, E., Raisbeck, G., Yiou, F. and Jouzel, J.  2000.  Solar irradiance during the last 1200 years based on cosmogenic nuclides.  Tellus 52B: 985-992.

Cliver, E.W., Boriakoff, V. and Feynman, J.  1998.  Solar variability and climate change: geomagnetic and aa index and global surface temperature.  Geophysical Research Letters 25: 1035-1038.

Hoyt, D.V. and Schatten, K.H.  1993.  A discussion of plausible solar irradiance variations, 1700-1992.  Journal of Geophysical Research 98: 18,895-18,906.

Lal, D. and Peters, B.  1967.  Cosmic ray produced radio-activity on the Earth.  In: Handbuch der Physik, XLVI/2.  Springer, Berlin, Germany, pp. 551-612.

Lean, J., Skumanich, A. and White, O.  1992.  Estimating the sun's radiative output during the maunder minimum.  Geophysical Research Letters 19: 1591-1594.

Lean, J., Beer, J. and Bradley, R.  1995.  Reconstruction of solar irradiance since 1610: implications for climate change.  Geophysical Research Letters 22: 3195-1398.

Nesme-Ribes, D., Ferreira, E.N., Sadourny, R., Le Treut, H. and Li, Z.X.  1993.  Solar dynamics and its impact on solar irradiance and the terrestrial climate.  Journal of Geophysical Research 98 (A11): 18,923-18.935.

Pang, K.D. and Yau, K.K.  2002.  Ancient observations link changes in sun's brightness and earth's climate.  EOS, Transactions, American Geophysical Union 83: 481,489-490.

Raisbeck, G.M., Yiou, F., Jouzel, J. and Petit, J.-R.  1990.  10Be and 2H in polar ice cores as a probe of the solar variability's influence on climate.  Philosophical Transactions of the Royal Society of London A300: 463-470.

Reid, G.C.  1991.  Solar total irradiance variations and the global sea surface temperature record.  Journal of Geophysical Research 96: 2835-2844.

Reid, G.C.  1997.  Solar forcing and global climate change since the mid-17th century.  Climatic Change 37: 391-405.

Rigozo, N.R., Echer, E., Vieira, L.E.A. and Nordemann, D.J.R.  2001.  Reconstruction of Wolf sunspot numbers on the basis of spectral characteristics and estimates of associated radio flux and solar wind parameters for the last millennium.  Solar Physics 203: 179-191.

Solanki, S.K. and Fligge, M.  1998.  Solar irradiance since 1874 revisited.  Geophysical Research Letters 25: 341-344.

Zhang, Q., Soon, W.H., Baliunas, S.L., Lockwood, G.W., Skiff, B.A. and Radick, R.R.  1994.  A method of determining possible brightness variations of the sun in past centuries from observations of solar-type stars.  Astrophysics Journal 427: L111-L114.