ding
You want an experiment to directly measure the LWave IR back radiation from A REAL SKY anywhere in the world? At LEAST 80 studies out there that do exactly that. That cuts your goalpost for experimental evidence at least in half.
You can stop laughing when they attribute everything they measured to a 22 ppm change in the amount of CO2 between start/end of the measurements. LOL. ALTHOUGH the CO2 very likely was a major contributor.
There are others like this that measure the back rad (reflected radiative heat) from the GHouse.
The climatic impact of CO2 and other greenhouse gases is usually quantified in terms of radiative forcing, calculated as the difference between estimates of the Earth's radiation field from pre-industrial and present-day concentrations of these gases. Radiative transfer models calculate that the...
pubmed.ncbi.nlm.nih.gov
Observational determination of surface radiative forcing by CO2 from 2000 to 2010
D R Feldman 1, W D Collins 2, P J Gero 3, M S Torn 4, E J Mlawer 5, T R Shippert 6
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PMID: 25731165 DOI: 10.1038/nature14240
Free article
Abstract
The climatic impact of CO2 and other greenhouse gases is usually quantified in terms of radiative forcing, calculated as the difference between estimates of the Earth's radiation field from pre-industrial and present-day concentrations of these gases. Radiative transfer models calculate that the increase in CO2 since 1750 corresponds to a global annual-mean radiative forcing at the tropopause of 1.82 ± 0.19 W m(-2) (ref. 2).
However, despite widespread scientific discussion and modelling of the climate impacts of well-mixed greenhouse gases, there is little direct observational evidence of the radiative impact of increasing atmospheric CO2. Here we present observationally based evidence of clear-sky CO2 surface radiative forcing that is directly attributable to the increase, between 2000 and 2010, of 22 parts per million atmospheric CO2. The time series of this forcing at the two locations-the Southern Great Plains and the North Slope of Alaska-are derived from Atmospheric Emitted Radiance Interferometer spectra together with ancillary measurements and thoroughly corroborated radiative transfer calculations.
The time series both show statistically significant trends of 0.2 W m(-2) per decade (with respective uncertainties of ±0.06 W m(-2) per decade and ±0.07 W m(-2) per decade) and have seasonal ranges of 0.1-0.2 W m(-2). This is approximately ten per cent of the trend in downwelling longwave radiation. These results confirm theoretical predictions of the atmospheric greenhouse effect due to anthropogenic emissions, and provide empirical evidence of how rising CO2 levels, mediated by temporal variations due to photosynthesis and respiration, are affecting the surface energy balance.