La Niña continued to gain strength in November as we approach the normal peak for these events in the Northern Hemisphere winter—usually November–January. Forecasters estimate at least a 95% chance that La Niña will last through the winter, with a potential transition to ENSO-Neutral during spring 2021 (~50% chance).
La Niña sticks out like a sore thumb when taking a gander at a map of sea surface temperature anomalies (the difference from the long-term average) over the Pacific Ocean. The Niño3.4 region of the tropical Pacific (the area we look at for determining ENSO status) was much cooler than the La Niña threshold of -0.5°C, at -1.4°C below average for November according to the ERSSTv5 dataset. In fact, the Niño3.4 region surface temperature anomaly has been lower than -1.0°C for the last two months, and the November anomaly was the seventh-lowest of all Novembers going back to 1950.
In the Tropical Pacific Ocean Lane, the Ocean-Atmosphere is glistening
As always, if we want to see if this La Niña is humming along, we’ll need to take stock of how well our oceans and atmosphere are working together. During La Niña, the expectation is that there will be less rain than average over the central Tropical Pacific Ocean and more rain over the Maritime Continent in Indonesia and the Philippines. This pattern can be seen in looking at changes in the amount of radiation leaving Earth into outer space, which can be detected by satellites.
Clear skies let outgoing longwave radiation (OLR) escape into space. But clouds act like a bouncer, blocking the energy from entering Club Outer Space and telling it to go home. Less OLR reaching the satellite means more clouds and more rain. More OLR means the opposite, sunnier skies and less rain. During November, we saw less rain over the Date Line, but the Maritime Continent rainfall was largely near average (we aren’t sure why, but the expected enhanced rainfall has had trouble sticking around during this event).
Another key signal to how well La Niña is doing lies in the wind. ENSO events disrupt the Walker Circulation, the normal atmospheric wind pattern that blows across the tropics.
La Niñas tend to rev up the existing Walker Circulation. The trade winds, which blow east to west across the Pacific Ocean, blow a little harder, while winds higher up in the atmosphere blow to the east a little bit harder. During November, that is exactly what happened. (For more information on how this is part of a feedback mechanism that gets La Niña going, check out Michelle’s recent post.)
Simply put, this is my long way of saying that this La Niña is looking like a La Niña.
In the Pacific meadow, we can build a forecast
The big question now is how long this La Niña will last. And while we’ve looked a lot at the atmosphere and the ocean surface, to answer that question it’s useful to take a look under the surface of the Tropical Pacific Ocean.
There you’ll find plenty of cooler-than-average water across the central and eastern Pacific Ocean. This fount of coolness is (1) a sign of the atmospheric/ocean coupling that I described above and (2) plenty big and strong enough to provide a source for cooler than average water at the surface over the next several months. Although, it is important to note that this fount of cooler than average anomalies in the subsurface ocean has weakened slightly over the last month compared to October.
That small weakening might be a harbinger for the future of this event. Most of the computer models we use as well as the forecasters predict La Niña to last through winter (greater than a 95% chance). But, forecasters do not expect much more strengthening, with the event peaking between -1.0°C to -1.5°C for the seasonal average Niño3.4 surface temperature anomaly (often referred to as “moderate”). After which, the forecast is for La Niña to weaken throughout the spring (~50% chance of ENSO-Neutral during April-June).
As with any forecast six months into the future, there is still plenty of uncertainty as to the eventual path this La Niña takes. But don’t worry, because as those computer model ENSO Bells ring, we’ll be listening. (Is that taking this month’s Winter Wonderland theme too far? No? It’s a beautiful sight? You’re happy tonight? I’ll stop now.)
Gone away are the blue colors (cold anomalies). Here to stay are the red colors (warm anomalies)
La Niña isn’t the only thing happening across our planet, even though it really sticks out on a map of ocean temperature anomalies. Of course, one reason why it sticks out is that everywhere else is so much warmer than average. Because even as La Niña formed this year, on a whole, 2020 has been sizzling hot.
Usually, years with La Niñas are cooler than years without due to the huge amount of cooler than average ocean water exposed across the equatorial Pacific. On the flip side, years with El Niños tend to fall on the warm side. For instance, the warmest year on record is 2016 when one of the strongest El Niños since 1950 occurred. Meanwhile, the coolest years of most decades coincide with a La Niña.
And that got me thinking. How do this year’s global temperatures compare to global temperatures in similar years when a La Niña developed in the summer/fall after lukewarm conditions during the preceding winter?
Going back to 1950, there have been only seven cases that sort of matched—1954, 1964, 1970, 1988, 1995, 2007, 2010—and of those, four (bolded) were the closest matches. Comparing the closest matches, 2020 is on track to be almost 0.5°F warmer than the next warmest (2010) and 1.6°F than the coolest year. While that doesn’t seem like much, it is the difference between being ranked as the first or second warmest year on record (2020) or the seventh (2010) or #59 (1970). Clearly, the warming trend due to human-caused climate change is helped to bump up global temperatures over time. And 2020 is no exception. But even then, 2020 has certainly been something else.
Emily will be back later this month with the last ENSO Blog post of 2020, but don’t worry—we’ll still be here in 2021, giving you all the latest news on ENSO.