This post contains three addenda to the next post; additional/further explorations that I feel have more of a tangential than a fundamental bearing on the main argument laid out there, still, I would say, providing some definite extra depth, scope and context to it. The figure numbering here will simply carry over from the main post (ending with number 31.), and all figures referred to in the text or captions below (but not in direct quotes) numbered somewhere between 1. and 31. will be from that post, unless otherwise noted.
The three addenda are:
I – A net flux composite
II – What do the models say?
III – ASR and cloud albedo
”The main tool used in this study is correlation and regression analysis that, through least squares fitting, tends to emphasize the larger events. This seems appropriate as it is in those events that the signal is clearly larger than the noise. Moreover, the method properly weights each event (unlike many composite analyses). Although it is possible to use regression to eliminate the linear portion of the global mean temperature signal associated with ENSO, the processes that contribute regionally to the global mean differ considerably, and the linear approach likely leaves an ENSO residual. We have shown here that 0.06 °C of the warming from 1950 to 1998 can be accounted for by the increased El Niño phase of ENSO. The lag of global mean temperatures behind N3.4 is 3 months, somewhat less than found in previous studies. In part, this probably relates mostly to the key ENSO index used, as the evolution of ENSO means that greater or lesser lags arise for alternative indices that also vary across the 1976/1977 climate shift.”
From Trenberth et al. 2002: “Evolution of El Niño-Southern Oscillation and global atmospheric surface temperatures.”
I want you to bear this quote in mind – especially the highlighted part – throughout this post. Because what we will do in the following, is to address and track Trenberth’s ‘ENSO residual’, the result of ENSO-related oceanic/atmospheric processes operating and contributing regionally to global mean temps outside the ‘key ENSO index’ region in the equatorial East Pacific (the NINO3.4), and that evidently (according to the data) differ considerably in their effects (contributions) from some ENSO events to others. This extra-NINO part of the ENSO process is what caused ‘global warming’ since 1980. That’s not a claim. It’s an observation. It’s right there in the freely accessible real-world data. For all to see.
If one simply cares to have a look … And knows what to look for. Continue reading