December 16, 2018 - By Emily Becker - The surface of the tropical Pacific Ocean is nice and warm, but the atmosphere just doesn’t seem interested. Will these two crazy kids get in sync and qualify as El Niño conditions? Forecasters think there’s a 90% chance that will happen soon and continue through the winter.
Following our “Is it El Niño conditions?” decision tree, once we have a monthly average surface temperature anomaly in the Niño3.4 region above 0.5°C (currently near 1.0°C), and it’s forecast to stay that way for the next several months (it is; more on that later), we need signs of an atmospheric response before we can change our relationship status to “El Niño Advisory.”
While warmer-than-average surface waters in the equatorial Pacific are an essential element of El Niño, the atmospheric response is just as critical. In the case of El Niño, those warmer-than-average waters in the central and eastern Pacific warm the air above them, leading to more rising air, clouds, and rain. So much more rising air, in fact, that the entire circulation over the equatorial Pacific—the Walker circulation—is changed.
The average Walker circulation is driven by strong rising air over Indonesia, leading to west-to-east winds aloft, sinking air over the Eastern Pacific, and returning east-to-west winds (the trade winds) near the surface of the Pacific. More rising air in the central and eastern Pacific weakens this circulation, slowing the trade winds along the surface. Like any good partner, the slower trade winds help to sustain El Niño, keeping the surface waters warmer.
A mysterious stranger
What’s distracting the atmosphere from settling down with the ocean into El Niño? Perhaps it’s a subseasonal dalliance! (Yep, I’m going to torture this metaphor. Buckle in.) We’ve covered The Madden-Julian Oscillation (MJO) a few times before in this space. The MJO is a major area of rising air, clouds and rain (“enhanced convection,” if you’re feeling frisky) that moves eastward along the equator, affecting global atmospheric circulation. It can circle the globe in about 4–6 weeks. It’s also a great cook, and loves long walks on the beach.
The MJO has been active over the past few months, circling the Earth a few times since September. When the MJO-related area of enhanced convection moves from Africa to the Indian Ocean and through the Pacific, it changes the winds and cloud patterns in the areas we monitor for El Niño conditions. The MJO is a subseasonal pattern, meaning it affects conditions on timescales of a few weeks. Recently, most of the changes we’ve observed in the atmospheric circulation over the tropical Pacific look MJO-related, changing from week to week.
ENSO, on the other hand, is a seasonal pattern, meaning it lasts for several months in a row. We’ve already observed a season of above-average tropical Pacific surface temperature and expect it to continue through the spring. When the atmospheric response to the warmer-than-average waters has kicked in, those signature changes (the weak-in-the-knees Walker circulation) will lock in for the long haul. The consistent changes in the atmospheric circulation are how El Niño affects global weather and climate patterns.
You are my density
There’s a 90% chance that El Niño conditions will form soon and last through the winter, with a 60% chance it will last through the spring. Why are forecasters confident that these two are destined for each other? Most climate models predict that sea surface temperatures will remain higher than the El Niño threshold (0.5°C above average). Adding support to this is that the amount of warmer-than-average water under the surface is still quite high, although slightly decreased from last month (the November average tied for sixth highest since 1979). This will provide a source of warmer-than-average water for the surface over the next few months.