Considering that a hundred examples can be easily made to the efficacy of one dimensional models in physical systems, and another hundred of the needless complexity of the general category of 3D models in given situations, your argument is flat incorrect.
Care to be more specific? Are any of these systems the atmosphere? If not, explain how they apply in this instance.
The atmosphere is both 3D and dynamic and generally speaking, history has taught us that the more detailed you can make model, the better. This applies to climate, weather prediction, air quality forecasts, whatever.
Seems like an odd leap to lump a use of the virial theorum with "one dimensional" , to boot.
I didn't just dream that you know. This is taken from the paper:
In this paper we derive purely theoretical relationships between the above quantities by using a simplified one dimensional atmospheric radiative transfer model.
What you've left out of your comment and which misrepresents the two means of looking at phenomena is the restrictions and/or limitations placed on the utility of the results by those making (whichever) respective argument.
Perhaps you'd like to comment then, and explain why a 1D model is so much more suitable for this system?
Thus your critique as phrased may be considered laughable nonsense.
I'm sure you have that opinion. I have my own about what you've just said as well.
I suspect that Miskolczi discussion is quite beyond JREF, it is quite technical.
It also seems to be quite beyond most high-profile journals as well. Why exactly was such groundbreaking research published in such an obscure journal? No disrespect to the Hungarian Meteorological Service but
IDŐJÁRÁS isn't exactly
Nature.
But hey, the floor is yours. Educate us. Explain why Miskolczi's model gets it right while all the others fail.
ETA: I might add that this is something that Miskolczi didn't do; all he did was effectively say, "here's my model, which
should work. It replicates some real-world data, therefore it
must work", which isn't a closure or validation by any stretch.