The maps below show the results, with the height of the columns corresponding to the number of years in each category. Warmer than average conditions are definitely favored in most Alaska locations in El Niño summers, and dry conditions are more common than wet from Anchorage to Nome, Kotzebue, and Barrow; but elsewhere (including in Fairbanks) the precipitation patterns are mixed.
We know that the phase of the Pacific Decadal Oscillation (PDO) is also a very important influence on Alaska climate, so I then subdivided the top 20 El Niño years by whether the PDO was positive or not. Compare the two maps below: the first shows the climate for nine years with both El Niño conditions and a significantly positive PDO phase, but the second map shows El Niño conditions combined with a near-neutral or negative PDO phase. The difference is stark; unusual warmth is strongly favored in southern and central Alaska when the "warm" PDO phase lines up with El Niño, but a cool summer is actually more likely in the southwest in El Niño years with a neutral or negative PDO.
The corresponding precipitation maps are shown below; the dry signal is strong from the west coast to Fairbanks and Anchorage in the El Niño - positive PDO years, but a less positive PDO phase creates a more variable pattern.
These results suggest that the PDO phase is more important than ENSO for summer temperatures over Alaska, because the El Niño signal is largely removed when the PDO is neutral or negative. The maps below, derived from the top 10 positive PDO summers, confirm that the PDO temperature signal is stronger than the El Niño temperature signal, when taken in isolation. Thus a strongly positive PDO phase is more reliably connected to summer warmth than El Niño, and the Fairbanks summer is also more likely to be dry in positive PDO years.
What does all this mean for summer 2014? Well, the El Niño part is just speculation, because El Niño hasn't even developed yet, let alone a strong El Niño. However, the PDO has been significantly positive for several weeks now, as the long-lived pool of warm water in the North Pacific has moved closer to the west coast of North America. If this pattern persists, which seems quite likely, then the positive PDO signal will come into play and another warm summer will indeed be on the cards.
Very good analysis Richard. Have you looked at the lag time for the PDO correlation in June/July? For example, does the positivity of the PDO take a number of weeks or months to affect the climate or is it concurrent. I'm just thinking out loud and am not suggesting additional analysis.ReplyDelete
Brian, I haven't looked at any lagged effects yet. The analysis was based on the concurrent PDO phase, i.e. June-July mean PDO index compared to June-July weather conditions. To make a forecast in the true sense, I would need to look at how March PDO is correlated with summer conditions. Perhaps I'll try that soon.ReplyDelete
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Richard, is there any way that i could get you take a look at April and May instead of June and July??? I'm thinking that the graphs would be somewhat similar, and would go a long ways in helping to predict breakup activities in Alaska, but i just want to be sure. Nice work!!!Delete
Eric, it shouldn't be difficult, I'll see what I can do!Delete
I added a new post on the subject - see the home page.Delete
I read the graphs that the El Nino signal was weak and not zero. It seems that El Nino is important when the PDO is weak or negative and not important when the PDO is positive. The PDO overwhelms El Nino. This makes sense to me with El Nino being equatorial but maybe more potent and PDO being "weaker" but closer to Alaska. Weather is a funny thing.ReplyDelete
Great blog! I am wondering what an Alaskan winter with a positive PDO in an El Nino year would look like. Or what about a negative, or neutral PDO? Thanks!ReplyDelete
Tracy, thanks for reading. I'll create the autumn and winter PDO/ENSO maps soon and make a new post.Delete