Observational Evidence for the Greenhouse Effect
In a previous post I looked at evidence of the greenhouse effect from empirical data. In short, an analysis of empirical data for CO2 and GMST shows a one-way causation with CO2 causing warming since the mid-twentieth century. This paper conclusively establishes causation from empirical time series of CO2 and temperature. That is, not only is CO2 a good predictor of temperature, but uncertainty is reduced in future values of temperature given past values of CO2. This evidence is conclusive, but even without this, we have observational evidence for the greenhouse effect. In this post I want to consider how this is true generally in satellite observations of earth's emission spectrum at the top of the atmosphere and in individual studies that have made observational determinations of the greenhouse effect.
General Observations
The graph above quite literally shows the greenhouse effect. This can be readily determined, but we need to begin by calculating the effective temperature of earth with empirical data. The equation is:
Tp = Ts√(Rs√[(1-α)/ε]/2D) where:
Ts = 5778 K (temperature of sun)
Rs = 6.96x10^8 m (radius of sun)
D = 1.496 x 10^11 m (distance to sun)
α = 0.306 (albedo of earth)
ε = 1 (emissivity of earth)
Tp = 255 K or -18 C
This is fairly standard and not controversial. If the earth was had no atmosphere, the average surface temperature of the earth would be about -18 C. However, we know that currently, the earth is about 33 C warmer than this, even though I'm using current values for Ts and α. This means necessarily that neither solar variability nor changes in albedo can explain why the earth is 33 C warmer than its effective temperature. It's neither energy entering the earth's climate system nor the amount of solar energy reflected back into space that can explain the discrepancy. The 33 C difference must be caused by something else, and the above diagram of the Earth's emission spectrum shows us what is causing the warming.
Studies from Top of the Atmosphere
To my knowledge the first study to provide an observational determination of the greenhouse effect was Harries et al 2001[1]. Harries compared outgoing longwave radiation from two orbiting spacecraft, allowing the comparison of observations from 1970 and 1997. Differences in the relevant spectral bands could then be attributed to rising GHG concentrations. The differences in the spectra point to changes in atmospheric CH4, CO2, O3 and CFCs, and provided "direct experimental evidence for a significant increase in the Earth's greenhouse effect." These measurements contained significant uncertainties, since satellites have difficulty distinguishing between instantaneous radiative forcing and the climate radiative response.[2] Nevertheless, this was probably the first observational confirmation of the theoretical expectations of the greenhouse effect.
Studies from the Surface
Feldman et al 2015 found observational evidence of the greenhouse effect by studying the increase in radiative forcing in two locations, one in Oklahoma and the other on the north slope of Alaska from 2000 to 2010. The clear-sky radiative forcing they measured showed "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."Conclusion
https://www.researchgate.net/publication/12065270_Increases_in_greenhouse_forcing_inferred_from_the_outgoing_longwave_radiation_spectra_of_the_Earth_in_1970_and_1997
[2] Jiang, Y., Aumann, H. H., Wingyee-Lau, M., & Yung, Y. L. (2011). Climate change sensitivity evaluation from AIRS and IRIS measurements. In Earth Observing Systems XVI (Vol. 8153, p. 81531Z). Proceedings of SPIE. International Society for Optics and Photonics. http://dx.doi.org/10.1117/12.892817
[3] Kramer, R. J., He, H., Soden, B. J., Oreopoulos, L., Myhre, G., Forster, P. M., & Smith, C. J. (2021). Observational evidence of increasing global radiative forcing. Geophysical Research Letters, 48, e2020GL091585.
https://doi.org/10.1029/2020GL091585
[4] Feldman DR, Collins WD, Gero PJ, Torn MS, Mlawer EJ, Shippert TR. Observational determination of surface radiative forcing by CO2 from 2000 to 2010. Nature. 2015;519(7543):339‐343. doi:10.1038/nature14240
https://escholarship.org/content/qt3428v1r6/qt3428v1r6_noSplash_b5903aebfe105b4071103e11197138f8.pdf
[5] Plass, G.N. (1956), The Carbon Dioxide Theory of Climatic Change. Tellus, 8: 140-154. https://doi.org/10.1111/j.2153-3490.1956.tb01206.x
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