Bruce,
I agree with the points that you make in your post, but now to get back to a review of the evidence available to us:
Due to NOAA's Toga-Tao buoy array the 1997-98-Super-El Nino event represents a unique case where we can look at real measured data (not computer model projections, which have limitations). Therefore, I am posting four (for April, May & September 1997 and for January 1998) of the Scripps subsurface temperature anomaly plots from the site that Csnavywx provided a link to (see figure captions and link below):
http://meteora.ucsd.edu/~pierce/elnino/en97/en97.htmlCaption for the first image: "In April of 1997, something interesting happened. El Niños grow because of an unstable interaction between winds and the ocean that works like this: if the ocean warms in the center of the Pacific (where "D" is pointing to in the picture), then the winds tend to get weaker there. But when the winds get weaker, the ocean gets warmer. Then the winds get weaker still, and the process keeps going. For the current El Niño, you first see this starting to happen around April of 1997."
Caption for the second image: "By May, it's starting to look like it's going to be a big El Niño. The warm patch in the center of the Pacific, the one you could see forming in April, has started expanding to the east. At the same time, the surface waters off Peru are starting to get unusually warm. The warm anomaly below the surface is quite strong, over 6 degrees Celsius (about 11 F)."
Caption for the third image: "By September 1997, a strong El Niño is underway. Surface temperatures are 2 to 4 degrees Celsius (4 to 7 degrees F) warmer than usual, starting at the coast of South America and stretching to the dateline -- that's a quarter of the way around the planet!"
Caption for the fourth image: "In January of 1998, the El Niño is fully underway. The cold anomaly in the subsurface western Pacific has also expanded towards the east; this may be an early sign of an upcoming cold-water event ("La Niña")."
While I believe that the 1997-98 Super El Nino potentially may not be as severe as a 2014-15 El Nino [for reason such as: (i) 1997-98 was in a period of decreasing PDO while 2014-15 is in a period of increasing PDO/IPO; (ii) the 2014-15 EKW is occurring about one month earlier and for the same location of EKW is already more intense than the 1997-98 EKW; (iii) the ocean-atmosphere positive reinforcement loop is starting about one month earlier in 2014 than in 1997; (iv) the amount of warm water stored in the Western Equatorial Pacific has a larger volume and is warmer in 2014 than in 1997; and (v) there are already forecasts that the 2014 typhoon season may begin about one month earlier than in 1997], and that the 1982-83 El Nino might actually serve as a better case study for a possible 2014-15 Super El Nino [as: (a) it occurred during a period of increasing PDO/IPO; and (b) the recently ended period of increased La Nina events had built-up a meaningful pool of warm water in the Western Equatorial Pacific], nevertheless, we only have good data for the 1997-98 Super El Nino event (which of course is the strongest El Nino in recorded history so it is a good case study). Therefore, I offer the following observations about the Scripps subsurface temperature anomaly images:
(a) As noted in the caption for the April 1997 image the stem of warm water labeled "D" near the dateline serves to initiate the positive ocean-atmosphere reinforcement that we are currently observing in March 2014, which is the signature indication that an El Nino event (mild or otherwise) is beginning. The fact that the maximum temperature anomaly in April 1997 was only about 4.5 degrees C while the max. temp. anomaly by the end of March 2014 is over 7 degrees C, is most likely due to the facts that: (a) the water moving eastward from the Western Equatorial Pacific is more voluminous and warmer than in 1997, (b) the Peru-Humboldt current off the coast of Peru is being slowed down sooner [& thus is sending less cold water westward] than in 1997 [the fact that a deep warm-water bulb of water exists of the coast of Peru/Ecuador below -250m water depth in March 2014 is an indication to me that the upwelling in this area is already being reduced because the 2014 EKW is so large that it ready reached the west coast of South America very early in the season so as to effect the Peru-Humboldt current very early]; and (c) the temperature anomaly is measured relative to the seasonal expected base temperature, so early arrival of the 2014 EKM has an effect on the temperature anomalies measured.
(b) The May 1997 subsurface temp. anomaly plot indicates that the PDO reinforcement in 1997 was comparable to (or less than) the current March PDO conditions as supported by the SST images that deep octopus posted for March 27 2014 (in Reply #384). I would expect the shape of the April 2014 subsurface plots to be similar to the May 1997 plot, except that I would expect the maximum temperature anomaly in April 2014 to be at least 2.5 degrees C higher [and possibly more] than in May 1997.
(c) The September 1997 plot shows a strong El Nino had already formed, and that NOAA certainly made this information available publically; and I would expect that it is possible that similar condition may occur in 2014 by August, thus possibly allowing NOAA and other agencies even more time to provide advance warning of an impending Super El Nino.
(d) The January 1998 plot shows a cold-water EKW moving westward, signally the coming of the La Nina that followed the 1997-97 El Nino event. While I believe that it is likely that if a Super El Nino occurs in 2014-15 that it will probably be followed by a La Nina; but depending on the Fall (austral Spring) IOD, it is possible that a 2014-15 Super El Nino could extend into 2016.