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The Temperature Feedback Problem

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  • Christopher Monckton

    (Science and Public Policy Institute 5501 Merchants' View Square, #209, Haymarket, VA 20169)

Abstract

In the past 810 ka, inferred variability of absolute temperature has barely exceeded ±3 K, or ±1 % of the period mean. This thermostatic behavior seems inconsistent with a feedback sum f t = (σ i f t,i ) ≫ 0 over any term of years t . In electronic circuits, as the loop gain g t exceeds 1, the Bode system-gain relation G t = (1 − g t ) −1 models the abrupt transition of the output voltage from V t → + ∞ to − ∞ ↠V t ( G t , V t being momentarily undefined at the singularity, where g t = 1). Yet in the climate, where g t might plausibly exceed unity owing to, say, the near-exponential Clausius-Clapeyron increase in the water-vapor carrying capacity of the atmospheric space as it warms, +Δ f t ⇒ +Δ T t ⇠−Δ T t for all f t > 0. In this and several other material respects the Bode relation, which as clearly specifies a negative dynamical-system response to g t > 1 as a positive response to g t

Suggested Citation

  • Christopher Monckton, 2015. "The Temperature Feedback Problem," Energy & Environment, , vol. 26(5), pages 829-840, September.
    • Handle: RePEc:sae:engenv:v:26:y:2015:i:5:p:829-840
    DOI: 10.1260/0958-305X.26.5.829
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    References listed on IDEAS

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    1. Simon Dietz & Chris Hope & Nicholas Stern & Dimitri Zenghelis, 2007. "REFLECTIONS ON THE STERN REVIEW (1) A Robust Case for Strong Action to Reduce the Risks of Climate Change," World Economics, World Economics, 1 Ivory Square, Plantation Wharf, London, United Kingdom, SW11 3UE, vol. 8(1), pages 121-168, January.
    2. Stern,Nicholas, 2007. "The Economics of Climate Change," Cambridge Books, Cambridge University Press, number 9780521700801.
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