Quote:
Originally Posted by Don C L
Hmmm... La Nina was supposed to give us a dry winter here in California... and THAT sure ain't happening!
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Indeed.
Despite La Niña’s (declining) presence, a robust series of storms brought impressive precipitation across California, spurring floods and landslides, increasing reservoir levels, and dumping eye-popping snowfall, in the mountains.
While La Niña and El Niño do factor into Southern California weather, another phenomenon, known as the
Madden-Julian Oscillation (MJO), can affect whether storms hit.
The MJO starts as a massive expanse of extra large precipitation, often in the form of tropical thunderstorms, that tend to move from the
Indian Ocean, eastward into the
Pacific Ocean. That can release an enormous amount of latent heat into the atmosphere, and through that action, it can influence storm tracks, and whether (or not) they hit California.
There can be multiple MJO
events within a season, and so the MJO is best described as intraseasonal tropical climate variability (varies on a week-to-week basis).
There’s also something called the
Quasi-Biennial Oscillation (QBO), which can disrupt the connection between the MJO, and weather on the
West Coast. The Quasi-Biennial Oscillation is a regular variation of the winds, that blow high above the equator. Strong winds (in the stratosphere) travel in a belt around the planet; and every 14 months or so, these winds completely change direction. This means a full cycle takes roughly 28 months, making it the most regular slow variation in the atmosphere, after the cycle of the seasons.
While the local weather effects from El Niño and La Niña usually happen (until they don’t), the bottom line is that, if you count every El Niño as wet, and every La Niña as dry (in California), sooner or later, you’re gonna get embarrassed.
It appears that climate & weather are slightly more complicated. than might be imagined, by a
single (or even 3) indicator(s).