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    <gco:CharacterString>STUDY NOTES: Two Antarctic records of Be-10 concentrations covering the last millennium are normalized and averaged in order to smooth out non-forced variability. This stack is corrected for geomagnetic variations and converted into solar modulation parameter PHI and total solar irradiance (TSI) over the period of years 695-1982 AD. Stack of Be-10 Antarctic records published by Raisbeck et al. 1990 and Horiuchi et al. 2008, using the C-14 adjusted timescale for the latter. The stack is corrected for geomagnetic variations reconstructed by Korte et al. 2009 with the production sensitivity of Wagner et al. 2000. The solar modulation parameter PHI is calculated following McCracken et al. 2004 method, i.e. by calibrating the stack to an average level of 645 MV over the period 1944-1966 AD. The sensitivity of the Be-10 production to PHI is from Webber and Higbie 2003, assuming that Be-10 is produced at 70% in mid-latitudes and 30% locally (&quot;mix&quot; case) or purely locally (&quot;local&quot; case). Total Solar Irradiance (TSI) is calculated from either of the PHI time series, assuming an average modern maximum of 1365.5 W/m**2 (year 1969 AD) and a 0.08% decrease at the Maunder Minimum (year 1692 AD) (most likely value of IPCC AR4 p.192). 
ABSTRACT SUPPLIED BY ORIGINATOR: Beryllium-10 in ice provides a valuable proxy of solar activity. However, complex production pathways, atmospheric transport, and deposition processes impede its quantitative interpretation. Here, we examine the influence of deposition processes on two Be-10 ice core records from Central Antarctica (South Pole and Dome Fuji stations), covering the last millennium. We try to quantify how Be-10 variations in ice relate to variations in Be-10 production, and the bias associated to this relationship. An independent bias estimation is provided by comparing atmospheric radiocarbon variations reconstructed from tree rings and deduced from Be-10 variations. Both techniques suggest an uncertainty of the order of 10% in Be-10 production. This uncertainty estimate does not account for the geographical origin of Be-10, which remains a major issue. Because both Be-10 records are so similar, we propose to average them as a means to decrease the unshared (non solar) variability. This average record provides a new reconstruction of solar modulation parameter PHI and total solar irradiance over the last ~1,300 years. The lowest solar activity is found during the so-called Spörer Minimum (around AD 1450). The highest activities are found during the 8th century and over the last decades: as shown in previous studies, our results suggest that the recent solar activity is not exceptionally high for the last millennium.</gco:CharacterString>
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