WxMidwest, on 8 April 2012 - 11:31 PM, said:
I don't know about that, ENSO is based upon the idea upwelling colder water from further depths, not just SST's by themselves, even during warmer periods Oscillations like this have still occurred. It's not like SST's will rise and Peristent Nino conditions will just stay put. Our climate system is dynamic.
The deep oceans have and will continue to warm as well (which is the primary reason for sea level rise), albeit at a slower rate than surface SSTs. Even if 3.4 region SSTs warm, it wouldn't necessarily lead to a persistent Nino-like state because the weather will primarily be determined by SST gradients. As long as 3.4 SSTs are cooler than the surrounding the weather will probably resemble more of a Nina like state. In short, warmer 3.4 SSTs do not necessarily = persistent Nino. Which is why NOAA is now going to use a sliding 30 year base period. This captures the dynamic variation you speak of. When 3.4 SSTs drop below the most recent 30 year base it will be classified as a Nina, when they rise above, it's a Nino.
They could also have changed the index to use global SSTs as a baseline rather than region 3.4 SSTs. That's how the PDO has always been calculated. If global SSTs rise 1C, so does the PDO baseline. That might not work as well for ENSO though since upwelling is so intense which may lead to a slower warming trend.