How is the accumulation of heat energy in the ocean good for us?
The last time the Pacific Decadal Oscillation reinforced global warming was 1998, and we had a spike in heat that was way above the average, higher than any year before it in the global temperature record. Some 15 years later, we are in a cold phase of the PDO and that record-breaking year is now pretty average, just one of the bunch. What happens when the PDO swings back to its atmospheric warming phase? How high do you think *that* spike will get? And how high do you think the average temp will be 15 years after that? How long can the temperature keep ratcheting up like this? After all, the PDO is cyclic, so it shifts between La Nina and El Nino. What will the next several shifts bring?
Apologies, Tomcat, for sloppy writing. I do know the general difference between short-term and longer term variations. I should know better by this point to write things while I'm half-asleep. Let me use the original ending, before it made sense to me to put in that offending 9 word phrase:
"After all, the PDO is cyclic. What will the next several shifts bring?" Now would you take a stab at answering the question? ;)
Exactly, Gryph. If the last go-around gave us the highest temps we've seen in many thousands of years at least, what happens the next time things line up like '98? How high will our atmospheric temps be when that heat starts coming out of the oceans and those El Nino winds start blowing? And how many more times will that happen? I suspect we're going to see more record-hot years in the future, and they will drift down to decadal average in 10 - 20 years. Of course, now I'm answering part of my own question. And I know what I think, usually. ;)
Thanks, Al! Finally a good answer!