Southern California is usually dependably uber-dry during July, helping make it the "golden state." But not this year. While the Pacific Northwest has been very dry this summer, southern California is enjoying lots of rain, leading to localized flooding and even the destruction of part of Interstate-10. The Los Angeles Angels' had their first rainout in 20 year, the San Diego Padres' had the first rainout since 2006, and Los Angeles enjoyed the wettest July day (.36 inches) in 130 years. July rainfall records are falling all over CA.
Let's explore what has happened and why. First, take a look at the percentage of normal rainfall during the last month. Some places in southern CA had over 800% of normal (which is admittedly a small amount). And Washington and western Oregon have been MUCH drier than normal (but admittedly we generally don't get much this time of the year). Our long range models very skillfully predicted this pattern months ago. Very impressive.
To get a different perspective, here is the precipitation over the past seven days over southern CA--very wet for this time of the year, with several locations securing daily or monthly 24-h records. Some locations in the mountains got hit by roughly 3 inches.
The last 24-h....more rain! Here are the 24-totals ending 11 PM Monday over southern CA. A number of mountain locations enjoyed more than an inch. All this rain is very welcome and helps lessen the fire danger, as well as reducing water needs for irrigation.
So what is going on? Why is southern California hugely wetter than the Pacific Northwest? During the last few days, the precipitation has been the result of the weakening Hurricane Dolores. Two days ago, the moisture advancing ahead of the storm brought thunderstorms and rain to Monterrey and the central coast (see below)
And today, as the weakened low center of Dolores was just offshore of Southern CA, moisture streamed over the southern CA coastal zone. Why was Dolores able to come so far north? One reason is the unusually warm water over the eastern Pacific this year.
There is substantial evidence that the most important cause of the southern CA precipitation is the surging El Nino, which tends to bring stronger upper level flow into the region. Here are the upper air (200 hPa) wind anomalies (differences from normal) for the past two weeks. Stronger than normal westerly and southwesterly flow into the upper Baja and the SW U.S. A split flow west of the Northwest. Classic El Nino signal.
The El Nino is rapidly strengthening....this may well be an historically strong event. California needs to prepare for a wet winter and we need to be ready for a boring one.