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λCO2 = z ln(o) / dTλ ≈ 5.35 ln(1.16) / 3.2 ≈ 0.25 W m-2 K-1. (6) The CO2 feedback completes the feedback-sum b: b = 1.8 - 0.84 + 0.26 + 0.69 + 0.25 ≈ 2.16 W m-2 ºK-1. (7) From κ = 0.313 and b = 2.16, a central estimate of the value of the feedback factor f is - f = (1 - bκ)-1 ≈ (1 - 2.16 x 0.313)-1 ≈ 3.077 (8) This result is broadly consistent with Hansen et al. (1984), where f = 3-4 is suggested. Final climate sensitivity ΔTλ, after taking accou
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