Rapid transition from record warmth & dryness to very wet pattern
February was an extremely warm month (once again!) across the entire state of California, with a seemingly endless list of temperature records being broken on a daily basis. February was also quite a dry month across the state, with essentially the only precipitation event of any note occurring around the middle of the month. Sierra Nevada snowpack–which had been hovering slightly above average through the end of January–started to fall behind by mid-month, and March 1st snow survey showed statewide snowpack slightly above 80% of average for the date. This number is decidedly far better than during recent winters, but that’s really only a testament to the abysmal snowpack accumulations during the reign of the Ridiculously Resilient Ridge. A rather abrupt change in the prevailing weather pattern is now at California’s doorstep, however. The persistent ridging of the past month or so is rapidly being displaced by a series of powerful storm systems, driven by a remarkable enhancement and consolidation of the Pacific jet stream.
One-two punch this weekend; intense rain, gusty winds, thunderstorms possible
Rain has already begun across the northernmost portion of California, and will continue more or less continuously through Monday. Precipitation will gradually spread further south on Friday and intensify on Saturday as a very strong cold front approaches the California coast. A robust atmospheric river (arguably of the Pineapple Express variety, given its subtropical origins near Hawaii) will be in place in advance of the front itself, providing plenty of moisture for the impressive larger-scale dynamics to act upon.
The nose of a strong jet streak will move inland over Central California before sagging southward over time, which is a favorable position for providing added lift as this storm system sweeps across the state from northwest to southeast. The very moist atmosphere combined with a fairly impressive frontal structure will likely lead to a period of very heavy rainfall across much of California. This setup would likely be cause for significant concern if antecedent conditions had been very wet, or if the front was expected to persist for a long period of time at a given location. Right now, though, the whole system appears to be fast-moving enough to prevent severe flood concerns–especially given our dry February. But given the high intensity of the expected precipitation, it will be worth watching closely to see if a frontal wave develops on Saturday and stalls the front more than expected. Should that occur, flood concerns would increase considerably.
In addition to fairly impressive upper-level dynamics for this part of the world, a substantial reservoir of cold air behind the cold front will provide quite a bit of instability during and after frontal passage–leading to a decent chance of at least isolated thunderstorms across much of the state beginning later on Saturday. Strong and gusty winds–perhaps in excess of 40 to 50 mph in some places–will also occur as surface pressure gradients strengthen.
A secondary system will develop rapidly late Saturday and early Sunday over the Pacific just west of California as the jet stream remains situated in an unusually favorable low-latitude position. While this surface low won’t have much time to develop before hitting the coast, it may still pack a substantial punch–particularly in Southern California. In fact, this second system could bring at least a brief burst of widespread heavy precipitation and perhaps fairly widespread thunderstorm activity to much of Southern California (focused from the Bay Area southward). There are some early indications that stronger surface-based instability could develop later Sunday or Monday across portions of Southern California, which (given strong jet dynamics) could lead to the development of some severe thunderstorm activity near the coast. Some stronger storms could also occur over some portion of the Sacramento/San Joaquin Valley on Sunday, depending on how much sun can poke through the clouds and further destabilize the atmosphere.
Rainfall totals through Monday across Northern California will be in the 2-4 inch range in most places (including San Francisco and Sacramento), with perhaps more than double that (5-8+ inches) in the coastal hills and the northern Sierra Nevada foothills. Most of Southern California will probably see rainfall more on the order of 1-2 inches, with double that in the coastal mountains. Notably, however, this precipitation will fall rather quickly, and may cause more problems that would typically be the case with precipitation of this magnitude. In the Sierra Nevada, snow levels will start out quite high as the warm atmospheric river moves ashore but will plummet later in the weekend as much colder air arrives. Several (2-4) feet of new snowfall is likely above 7000 feet, and lesser accumulations down to 4000 feet or so are likely by Monday as the secondary system moves inland.
Models have backed off on next week’s precipitation, but still bears watching
California weather (model) watchers got quite the show a couple of days ago when simulations started to suggest a relatively high potential for an extreme precipitation event to develop next week, following this weekend’s still very heavy rainfall. The setup was one strongly reminiscent of that which makes California water wonks nervous–the occurrence of a very persistent and strong atmospheric river event focused upon a narrow stretch of the West Coast. Several model cycles were hinting at the potential for truly incredible amounts of rain and high-elevation snow between March 4 and March 12.
Fortunately, however, it now seems that those really extreme numbers are unlikely to come to pass. While a very impressive atmospheric river is still expected to develop across the eastern Pacific next week and eventually make it to California, it is not presently expected to be nearly as persistent as had been simulated a few days ago. That said, though, the GFS and ECMWF both still agree that a strong storm will approach California later next week, dragging this atmospheric river onshore and producing at least modestly heavy precipitation. It’s possible that a wetter solution could yet re-emerge, and given this weekend’s virtually guaranteed heavy rainfall that will bear close watching. Present model solutions still suggest a storm that would be quite impressive by the low standards set during recent drought winters–so our newly-active pattern seems likely to continue for the foreseeable future.
A look (even further) ahead
In the longer run, it seems likely that a fairly active weather pattern will continue across California for much of March. It’s hard to say at this point whether precipitation this month might approach the remarkable late-season levels of the “Miracle March” in 1991, but it does at least appear likely that California’s snowpack will recover toward or even above average levels in the coming weeks. It’s less clear whether Southern California will be able to make up the seasonal precipitation deficit that has accumulated this year despite the near record-strength El Nino event in the tropical Pacific. Still, it appears increasingly likely that March will at least be able to make a dent–even though it’s quite clear that California’s multi-year drought will persist through the summer.
© 2016 WEATHER WEST