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It is not cherry picking and you know it.Now, why would my 40 year time period be cherry-picking but your 20 year time period not? Just because you picked yours first? That's ridiculous. You know that shorter times periods like yours are always more susceptible to noise than longer ones.
Sorry, long... but you ARE cherry-picking. Just like you repeatedly cherry-pick Karl et al.1993 out of all the studies about diurnal asymmetry to cite.
Not really. Karl et al.1993 was the first major study about this that was limited in its data. Only 37% of the Earth was covered and most of that was just the Northern Hemisphere. And I would remind you that ALL the studies that have been written about diurnal asymmetry since Karl et al.1993 show less to a lot less asymmetry. Why do you insist on pretending this is the only study to consider?
It Might. Might also have something to do with irrigation.
Oh... and you never did address Hansen's comments from that study you cited. Here it is again:
Are you planning on just ignoring this or do you think you could address it?
A much later study, Davies 2016, was a survey of the studies of diurnal asymmetry.
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In further Karl had the global asymmetry from 1951 to 2000 at T-Max .07C per decade,
and T-Min at .21C per decade, roughly the same ratio.
To show a continued trend, I would need to start where Karl ended, at year 2000!
The opening sentence of Davies 2016's conclusion stands in contrast to Hansen's statement.
Vs Hansen'sWhile there are many factors which may asymmetrically affect the radiative forcing on the diurnal extreme
temperatures, here, we demonstrate that the night‐time temperatures are inherently more sensitive to perturbations
to the radiation balance and will warm more rapidly on a uniform forcing (such as that from the build‐up of greenhouse‐gases).
If the models are expecting equal warming, and Hansen had a lot of input into the GCM models, then the models will run too hot!Thus the unrealized warming for greenhouse gases already in the atmosphere will appear almost equally in daily maximum and daily minimum temperatures.