This directory contains solar forcing functions for use in the PMIP3/CMIP5 simulations of the last millennium. For each reconstruction, we provide an estimate of the Total Solar Irradiance (TSI) as a function of year back to 850 CE, along with a high-spectral resolution estimate of the variations at individual wavelengths. There are multiple source datasets for these forcings, see descriptions below. Note that the extension of the quasi-11yr cycle and spectral characterstics of the reconstructions prior to 1610 (for the Delaygue/Bard (DB) and Muscheler et al (MEA) reconstructions) and for the spectral variations prior to 1850 for the Vieira, Krivova et al (VK) and Steinhilber et al (SBF) reconstrucitons are synthetic and added in for consistency of the forcing fields through time. Note that the DB and MEA extensions are scaled directly to the Wang et al (WLS) reconstructions back to 1610. The VK and SBF reconstructions are joined in 1849 since their Maunder Minimum values differ significantly from WLS. Note that the cosmogenic nuclide based reconstructions do not perfectly match the observed TSI changes from 1976 onwards and so, WLS are preferred for the post 1850 period. The synthetic 11 yr cycle is based on the average shape of solar cycles over the 20th Century in TSI from WLS, and the spectral characteristics are derived from a regression with TSI over the period 1610-2000 in the WLS spectral data. All reconstructions (except MEA) are calibrated to the WLS modern values (1976-2006) 1366.14 W/m2. Note that this is slightly higher than the PMOD composite of TSI over the same period which is 1365.96 W/m2 (a difference of 0.18 W/m2). The MEA record is more difficult to scale sensibly (though an inverse regression is used below). If a different calibration is required, we suggest a simple multiplicative scaling. Files: 1) Wang et al (1610-2000) tsi_WLS.txt (2 records) The Wang et al TSI reconstruction to 1610, with and without background changes. spectra_WLS_1610_2000_rescaled.txt From the original file spectra_1610_2000a_21Jan09.txt, with rescaled spectral values (so that the integral of the components equals the annual TSI). Slightly modified format (see notes below). spectra_WLS_1610_2000_rescaled_nobackground.txt An estimate of the spectral changes for the WLS no-background change case. This was calculated by scaling the 11yr smooth for each component so that the Maunder Minimum value was the same as the value in modern minima. This is provisional and may be superseded. Note that because this is estimated based on the w/background case, the TSI values are not exactly identical to the TSI nobackground case in the first file. 2) Delaygue+Bard extension (850-1609): spectra_DB_850-1609_background.txt spectra_DB_850-1609_nobackground.txt tsi_DB_lin_40_11yr.txt (2 records) extensions of the WLS solar reconstrucitons based on an Antarctic stack of 10Be records, scaled to the Maunder Minimum to modern changes in TSI seen in WLS and calibrated to the modern WLS value. The TSI values were derived by linear interpolation, a 40 yr smoothing and the addition of a synthetic 11 yr cycle. 3) Muscheler extension (850-1609): tsi_MEA_11yr.txt (two records) spectra_MEA_850-1609_background.txt spectra_MEA_850-1609_nobackground.txt 14C-based reconstruction, 40 yr smoothing, inverse regression to WLS over period 1630-1930, synthetic 11 yr cycle. 4) Steinhilber extension (850-1849): tsi_SBF_11yr.txt spectra_SBF_850-1849.txt TSI from 850 to 1849, scaled to modern WLS values. Synthetic 11yr cycle starting from the solar minimum in 1844. Join to WLS with/background data in 1850 for extension to the present day. 5) Vieira, Krivova extension (850-1849): tsi_VK.txt spectra_VK_850-1849.txt TSI from 850 to 1849 calibrated to modern WLS. 11 yr cycle already imposed. Join to WLS with/background in 1850 for extension to present day. 6) Figures: tsi.pdf TSI reconstructions from 850 CE to 2000 CE. Notes: - The average, normalised 11 yr cycle used had yearly components: (-0.786483,-0.299496,0.317166,0.636872,1.0,0.701905,0.342438, -0.0689046,-0.36599,-0.676228,-0.934423) (the TSI anomaly for any one year is the magnitude of the solar cycle, multiplied these coefficents added to the 40 year smoothed value). Note that the synthetic cycle is exactly 11 years. - the format of the spectra files is slightly different to the original file provided by Judith Lean. There is an extra line of text to prevent inadvertent confusion, but the main difference is that the spectral components are scaled so that the integral of the spectra is exactly equal to the TSI for that year. They can be read using the following fortran: integer, parameter :: nlean=3780,nyr=2000 character*80 title(7) real*8 wslean(nlean),fslean(nlean),spectra(nlean,nyr),tsi(nyr) real*8 year(nyr) integer :: yr1=1610, yr2=2000 ! change depending on file do i=1,4 read(1,'(A80)') title(i) end do read(1,'(5F14.2)') fslean read(1,'(A80)') title(5) do i=1,nlean/5 read(1,*) (wslean((i-1)*5+j),j=1,5) end do read(1,'(A80)') title(6) read(1,'(A80)') title(7) do n=yr1,yr2 read(1,*) year(n-yr1+1),tsi(n-yr1+1) do i=1,nlean/5 read(1,*) (data((i-1)*5+j,n-yr1+1), j=1,5) end do end do - Source data for the spectra and Wang and Lean TSI: http://www.geo.fu-berlin.de/en/met/ag/strat/forschung/SOLARIS/Input_data/CMIP5_solar_irradiance.html References: Lean J, "Calculations of Solar Irradiance" http://www.geo.fu-berlin.de/en/met/ag/strat/forschung/SOLARIS/Input_data/Calculations_of_Solar_Irradiance.pdf Delaygue, G and E. Bard. Solar forcing based on Be-10 in Antarctica ice over the past millennium and beyond', EGU 2009 General Assembly, # EGU2009-6943, http://meetingorganizer.copernicus.org/EGU2009/EGU2009-6943.pdf Muscheler, R., F. Joos, J. Beer, S.A. Müller, M. Vonmoos, and I. Snowball. 2007. Solar activity during the last 1000 yr inferred from radionuclide records Quaternary Science Reviews, Vol. 26, pp. 82-97. doi:10.1016/j.quascirev.2006.07.012 Steinhilber, F., J. Beer, and C. Frohlich, Total solar irradiance during the Holocene, GRL, 2009 Vieira et al, Wang, Y.-M., J. L. Lean, and N. R. Sheeley, Jr. (2005), Modeling the Sun’s Magnetic Field and Irradiance since 1713, ApJ, 625, 522–538, doi:10.1086/429689.