Daniel SwainThe following is an excerpt from a recent article on the
By Daniel Swain of Weather West
Extremely wet October in NorCal, then an extremely dry November…and a severe Western “snow drought”
The past 3 months have been, cumulatively, modestly wetter than average across NorCal, modestly drier than average across SoCal, record wet in parts of the Pacific Northwest, and record dry across portions of the eastern and southern Rockies. (climatetoolbox.org)
It has been a pretty interesting autumn, weather-wise, across much of North America. Record precipitation and severe flooding were observed in the Pacific Northwest and British Columbia; meanwhile, record warmth and dryness occurred across much of the interior West and Great Plains. In California, autumn 2021 proved to be a major departure from recent years, as a record-breaking atmospheric river event in October doused much of the northern half of state with extremely heavy rainfall that accounted for more than the entire average precipitation for the entire autumn season in just 2 days. Aside from that October event, though, precipitation has been very low statewide and temperatures have generally been well above average (except for some Central Valley folks stuck under a persistent layer of tule fog most days).
The net effect of all of this: California saw pretty minimal autumn wildfire activity due to relatively high soil and vegetation dampness and a lack of strong offshore wind events. NorCal saw some modest/partial drought relief, although precipitation deficits have further risen in SoCal. Accumulated precipitation from September 1 remains somewhat above average across much of NorCal (thanks to the big Oct. AR), but near or below average elsewhere following a long, multi-week dry spell during most of November into early December.
In a broader sense, the entire American West is presently experiencing a severe “snow drought” due to extremely warm (and, in many cases, also extremely dry) conditions this autumn. Snow water equivalent is well below average in every single major watershed from the Rocky Mountain Front Range to the Pacific Coast–a pretty extraordinary statistic. Interestingly, that includes PacNW watersheds that have actually received a lot of water this autumn–a product of warm atmospheric rivers that produced a lot of rain but very little snow due to high freezing levels. I do expect substantial improvement in this map along the Pacific Coast states over the next 2 weeks (including the Cascades and Sierra Nevada), although less so across the interior West.
Needed and welcomed precipitation on the (near-term) horizon
The good news is that there is a high likelihood of a major pattern change that will bring widespread rain (and mountain snow) to California over the next 10-14 days. A weak system moved in late Monday, bringing some local showers, but that’s likely to be just the appetizer. A second relatively weak system will move through CA on Thursday, bringing some more patchy light precipitation (which may actually skip much of NorCal, but bring some more substantial precip to parts of SoCal). But the real activity is slated to begin about 5-7 days from now, when a short series of cold and slow-moving storms may bring much more substantial rain and snow to the entire state.
At macro-scale, this pattern shift will be brought about by a retrogression (westward movement) of the persistent ridge axis near the West Coast to a position in the Gulf of Alaska. This will allow meridional flow and cold air to take up residence near the West Coast, allowing for a series of storms to affect California in the medium term. Right now, these look likely relatively cold (though not extremely so) systems that could be big Sierra snow producers and could, perhaps, allow for some foothill accumulations as well above 2,500-3,000 feet. It’s pretty likely that precipitation will be widespread across California, including the southern third of the state where rain and snow are much-needed following another dry autumn.
The upcoming wet pattern will be driven by a retrogression (westward movement) of the persistent/strong West Coast ridge. It’ll take up residence over the Gulf of Alaska instead, allowing colder storms to dive southward and affect California into mid-Dec.
Storms should help bolster very low snowpack and restore some streamflow
I am pretty optimistic that this pattern change, even if it ends up being relatively short-lived (as ensembles are hinting), could nevertheless greatly bolster Sierra snowpack over the course of just 7-10 days. 2-3+ feet of snow at Sierra pass level is possible over the next 10-14 days, and I would expect substantial (though lesser) accumulations at lower elevations as well. Widespread moderate to locally heavy precipitation is also plausible at lower elevations, hopefully raising streamflows and re-saturating the soils that have dried out since the big October AR.
Conditions will likely be cooler than average along the West Coast, though not exceptionally so. Meanwhile, an exceptional winter heatwave will develop across the eastern 2/3 of North America.
