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. 1997 Aug 5;94(16):8314–8320. doi: 10.1073/pnas.94.16.8314

Table 1.

Climate sensitivity estimates obtained by minimizing the RMSE between observed (IPCC) global-mean temperature changes and modeled changes over 1861–1994

Forcing
Raw IPCC data
IPCC data, ENSO removed
Low-pass filtered IPCC data
GHG Aerosol Solar ΔT, °C RMSE, °C R2 ΔT, °C RMSE, °C R2 ΔT, °C RMSE, °C R2
Yes 1.2 0.128 0.60 1.1 0.119 0.61 1.2 0.093 0.74
Yes Mid-IPCC 6.3 0.121 0.64 6.0 0.114 0.65 6.4 0.083 0.79
Yes Low 2.6 0.125 0.62 2.5 0.116 0.63 2.6 0.088 0.76
Yes Mid-IPCC Yes 3.0 0.117 0.67 2.8 0.107 0.69 3.0 0.077 0.82
Yes Low Yes 1.8 0.118 0.66 1.7 0.109 0.68 1.8 0.079 0.81

Results are given for five different forcing combinations and three different observed data series. The forcings used are IPCC GHG forcing; zero, central (Mid-IPCC), and “low” aerosol forcing (Mid-IPCC aerosol forcing is −1.3 W/m2 to 1990; low is −0.9 W/m2, a value that is substantially larger in magnitude than the IPCC lower bound); and solar forcing (33). The observed data cases are raw IPCC annual data; IPCC annual data with the ENSO influence factored out; and low-pass filtered IPCC data. The explained variance (R2) was calculated using R2 = 1 − (RMSE/SD)2, where SD is the standard deviation of the observed data (namely, 0.202°C for the raw IPCC data, 0.192°C for the data with ENSO removed, and 0.181°C for the low-pass filtered data).