I’m getting asked a lot of questions about our weather. Why are we getting so much rain? Why is it a year delayed from last year’s strong El Nino? Is the drought over? What’s going on?
To answer these questions I first have to give some perspective on climate in California and probabilities.
In case you don’t know, California is a state of extremes when it comes to precipitation. Throughout recorded history we’ve alternated between drought and excessive rain. Los Angeles is a good example of these extremes. While we average 15 inches of rain a year, we are rarely near this amount. If you look at the past 30 years, we’ve gone from extremely dry years to well above average years. In the end, it averages 15 inches.
The one question that is a little more difficult to explain is the why we’re getting the heavy rain this year instead of last year. Last winter we were prepared for the potential of heavy rain. The reason we thought this was because in all of the significantly strong El Nino climate patterns, Southern California got soaked. The odds were in our favor. But the rain didn’t come.
What is fascinating this year is we are in a weak La Nina or neutral weather pattern. Both of these patterns slant dry for the state of California and especially for Southern California. The probability our state would be dry this year is 70%, leaving a 30% chance we’d be above average. And, if you really study this image, there isn’t a weak La Nina pattern that is well above average for Southern California.
Instead what we are seeing is the wettest winter since 2010. The storms of the past two months have recouped 37% of the state’s five-year snow/water deficits. And for the first time since January 2014, no place in California is in an exceptional drought. Precipitation is more than 200% of average and the Sierra Snow pack is looking great!
So what gives? Why the two extremes in outcomes? I could give the answer, “That is how the weather works sometimes.” And this reply wouldn’t be completely wrong because even with an excellent forecast for a 90% chance of rain, there are days it’s dry.
But the answer is a little more complicated.
Last year the water was so warm in the Pacific that it affected the jet stream and moved all of the heavy rain to the Pacific Northwest and Northern California.
This winter we’ve been aided by numerous atmospheric rivers or a Pineapple Express. This type of pattern can occur at any time regardless of an El Nino, La Nina or neutral pattern. These rivers of atmospheric moisture are responsible for much of the devastating flooding in California’s history. And it played a big part in the flooding on Jan. 22.
Most people don’t know about the mega flood of 1862, which was caused by an intense atmospheric river. It has a return period of 100-200 years, meaning it will happen again.
And this leads me to climate change. The latest research shows that in a warming planet, droughts will become more severe and heavy rain events will occur more often. Before we started getting the rain in December, Southern California went through the driest five-year stretch ever recorded. And, if you look at tree ring data, it may have been the driest stretch in 1,000 years.
But if you look at the history of flooding in California, intense flooding events occurred before the industrial age and atmospheric rivers are responsible for most of these events. Attributing climate change to future flooding events may be hard to do. Upcoming research will need to address how a warming world affects atmospheric rivers.
Going forward, the key for our drought, especially in Southern California, is we need this kind of winter pattern for two more years so we can get out of a drought cycle. And, of course, I’ll keep you posted.