On the meaning of feedback parameter, transient climate response, and the greenhouse effect: Basic considerations and the discussion of uncertainties
Gerhard Kramm, Ralph Dlugi

TL;DR
This paper critically examines the commonly used energy balance models for Earth's climate, arguing they are flawed and do not convincingly demonstrate the atmospheric greenhouse effect when realistic data are considered.
Contribution
It provides a detailed critique of existing climate models, highlighting their physical inaccuracies and questioning the evidence for the greenhouse effect based on empirical data.
Findings
The globally averaged energy balance model is physically flawed.
The planetary radiation balance assumption is inappropriate without considering atmospheric effects.
Uncertainties in empirical constants overshadow the impact of anthropogenic forcing.
Abstract
In this paper we discuss the meaning of feedback parameter, greenhouse effect and transient climate response usually related to the globally averaged energy balance model of Schneider and Mass. After scrutinizing this model and the corresponding planetary radiation balance we state that (a) the this globally averaged energy balance model is flawed by unsuitable physical considerations, (b) the planetary radiation balance for an Earth in the absence of an atmosphere is fraught by the inappropriate assumption of a uniform surface temperature, the so-called radiative equilibrium temperature of about 255 K, and (c) the effect of the radiative anthropogenic forcing, considered as a perturbation to the natural system, is much smaller than the uncertainty involved in the solution of the model of Schneider and Mass. This uncertainty is mainly related to the empirical constants suggested by…
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