November 2016 La Niña update: Hello, lady!
Let’s take a tour through the La Niña diagnostic flowchart…
Is the sea surface temperature in the Niño3.4 region more than half a degree cooler than average? Yes! (It was about -0.7°C below average during October.) Do forecasters think it will stay cooler than that threshold for several overlapping three-month periods? Yes! (But just barely.) Finally, are there signs that the atmospheric circulation above the tropical Pacific is stronger than average? Yes! This all means that La Niña has officially arrived.
First things first
The Niño3.4 Index—the temperature of the ocean surface in a specific region of the equatorial Pacific, and our primary metric for measuring El Niño and La Niña—has been trending cooler since the demise of our big El Niño event in May. We now have two consecutive overlapping “seasons” (in climate forecaster lingo, that’s any three-month period) where the Nino3.4 Index averaged more than -0.5°C cooler than the long-term average: July—September and August—October.
One of the interesting things about this sea surface temperature map is just how warm the rest of the world’s oceans are, even compared to recent La Niña years like October 2011 or October 2007. Visit NOAA’s Visualization Lab to look at earlier years. (But be warned—there’s a lot of fun stuff to look at over there!)
The current NOAA Climate Prediction Center/IRI forecast gives La Niña conditions a slight edge through mid-winter: about a 55% chance. In order to qualify as a La Niña episode, La Niña conditions have to be present for at least five consecutive overlapping seasons, but of course we can’t know for sure in advance that that will happen. So, in order to qualify as La Niña conditions, we require a forecast that favors that they’ll remain for several months.
A 55% chance isn’t overwhelming, but not much about this La Niña is right now. Almost all of the computer models predict that the Niño3.4 Index will hover just below -0.5°C cooler than average for a few months, before returning to near-average in the late winter.
The final piece
The whole reason that ENSO (El Niño/Southern Oscillation) matters to countries located far from the tropical Pacific is the changes it causes to global atmospheric circulation. Therefore, we can’t have La Niña conditions without some specific changes in atmospheric circulation. There are several of these changes we look for, all related to the Walker Circulation over the tropical Pacific.
La Niña’s cooler surface waters lead to less rising air, and therefore fewer clouds than average in the central Pacific. Conversely, there is more rising air, clouds, and rain over Indonesia during La Niña. This part of the atmospheric response to La Niña has been pretty clear over the past couple of months.
We’ve also seen stronger-than-average easterly (blowing from east to west) winds in the central Pacific, more evidence that the Walker Circulation is strengthened. However, while this has been fairly consistent since mid-September, these winds are definitely not blowing us away!
The atmospheric response overall is fairly weak, going along with the borderline cooler sea surface temperatures of this La Niña… but it’s been consistent for a few months, meaning that we are seeing a change on seasonal timescales, and it’s time to formally welcome La Niña conditions! Be sure to check out Mike’s post to see what forecasters think La Niña means for U.S. winter weather.
The ENSO blog is written, edited, and moderated by Michelle L’Heureux (NOAA CPC), Emily Becker and Tom DiLiberto (contractors to CPC), Anthony Barnston (IRI), and Rebecca Lindsey (contractor to NOAA CPO). Posts reflect the views of the bloggers themselves and not necessarily Climate.gov, NOAA, or Columbia University/IRI.