It was one of those super-highs, stretching north to south rather than the usual west to east, that helped produce last year's big Antarctic blast.
That high was phenomenal, stretching from near the Antarctic ice shelf right over eastern Australia to Papua New Guinea. Between that huge high to our west and a deep low to the southeast of New Zealand we had the perfect air pressure machine to vacuum air from Antarctica and fire it as far north as the sub-tropics. Almost incredible.
When weather ambassador Bob McDavitt retired this summer from his long-held position as our government forecaster he parted with a comment that the highs around New Zealand were becoming more extreme.
He said earlier this year: "If the anticyclones are getting more extreme then that's going to impact on our seasonal forecast in the future.
"When the highs are getting more intense they also want to block and stop". If they stop and block to our west we get strong southerlies, as in August last year.
If they stall to our east then lows can be held up over New Zealand, as we we experienced in December with the flash floods in Nelson.
If they hold directly over us New Zealand gets starved of rain-makers as was the case in the summer of 2009. There was certainly something magical about the Antarctic blast last year, economic issues aside. But two years in a row may be too much of a good thing.