La Niña conditions reign in the tropical Pacific, with about a 90% chance of remaining through the winter. Get your popcorn and settle down on the couch—it’s time for this month’s ENSO cinema.
A recurring theme here at the ENSO Blog is the on-again, off-again relationship between the tropical Pacific Ocean and the atmosphere. ENSO (short for El Niño-Southern Oscillation, the entire El Niño–La Niña system) relies on the interaction between the ocean and the atmosphere. Average conditions in the tropical Pacific (see the drawing below) consist of relatively warmer surface water in the west and relatively cooler surface in the east. Air rises over the warm western water, forming clouds and rain; winds blow west-to-east high up in the atmosphere; air descends over the cooler east; winds blow east-to-west near the surface. Dun-dun-dunnn… it’s the Walker circulation!
When La Niña is present, the atmosphere takes one look at that characteristic cooler-than-average central/eastern Pacific ocean surface and gets all amped up. I haven’t yet seen the Walker circulation standing outside La Niña’s house holding a boombox aloft, but ENSO is always full of surprises.
The resulting stronger near-surface winds (the trade winds) reinforce the cooler ocean surface—the feedback mechanism fundamental to ENSO. For more on how this works, and a delectable bread analogy, check out Michelle’s Oscar-winning post.
All this is to say that La Niña conditions, after developing in September, continued in October. The surface of the ocean in the Niño-3.4 region, our primary ENSO-monitoring region, was about 1.0˚ C (1.8˚ F) cooler than the long-term average, via the ERSSTv5, our primary ENSO-monitoring dataset.
October featured La Niña’s atmospheric conditions—more rain than average over Indonesia, less over the central Pacific, and stronger-than-average trade winds over portions of the equatorial Pacific. As in all relationships, there are ups and downs, and these patterns were a bit weaker in October than in September. However, these two crazy kids are working on their relationship already, with a batch of stronger trade winds currently taking over much of the tropical Pacific.
“Predictable” isn’t high praise for a movie plot, but certainly is when it comes to the weather and climate. La Niña-related changes to global atmospheric circulation, including its effect on the jet stream, give us a picture of the average weather conditions expected over the next several months. To be clear, we mean the overall average, not that every day will exhibit the same weather!
There have been 23 La Niña events (24 counting this one!) in our historical record, which goes back to 1948. If we look at the October–December rainfall patterns during those La Niñas, we find more rain than average in northern California and the Pacific Northwest, and less than average through the Gulf coast and Southeast.
While La Niña tends to be linked to dry conditions and drought through California and the Southwest, that pattern usually develops in December–February through the early spring. You can step through the seasons to see ENSO impacts here. The strong atmospheric river that brought so much rain and snow to northern California last month was not atypical for a La Niña autumn. Overall, the October and early November North American rainfall map looked a lot like what we might expect this time of year during La Niña.
Will this La Niña, already a sequel itself, end up part of a trilogy? Three La Niña winters in a row aren’t unprecedented—that happened in 1973–1976, and 1998–2001—but it is relatively unusual. We will have a better idea by the late spring about what may happen with ENSO in 2022–2023.
Getting back to our current event, there’s about a 2-in-3 chance that this La Niña will be at least moderate in strength, meaning the peak Oceanic Niño Index (the 3-month-average Niño-3.4 anomaly) will be greater than 1.0°C cooler than average. The stronger the ENSO event, the more predictable the weather and climate impacts. More info about how we forecast the strength of an El Niño or La Niña event here.
Regardless of the critical reception, ENSO will always be bringing the drama, and your trusty ENSO bloggers will be here to watch and report!
This post first appeared on the climate.gov ENSO Blog and was written by Emily Becker.