Several media outlets and activist websites are claiming that this year's low snowpack is a major cause of the wildfires (see example below).
drying out grasses, trees, and shrubs that easily ignite and spread wildfires.
The facts are clear: such claims are wrong. The below-normal snowpack has had little impact in promoting recent wildfire activity.
To demonstrate this, let's consider the most impactful fire this summer, the Little Giant Fire near Lake Chelan, which was initiated by lightning on July 16 (see map below). The location of ignition (shown with a fire symbol) was at approximately 5000 ft.
We can get a good idea of snow evolution at the fire from the nearby Trinity Snotel site (see below).
The snowpack (snow water equivalent) at this location this year (black line) was generally below-normal (green line), but NOT a record low (lower red line).
If you look closely, the snowpack at this location melted out on May 2, when on average it melts out on May 11th. So, the snow was lost about 9 days early.
But that does not matter for this fire, since the fire occurred OVER TWO MONTHS (July 16). There is a large body of literature showing that only days to weeks are needed for surface fuels to become dry enough to burn after the snow has melted.
Furthermore, most of the water from snowmelt goes into streams and rivers and is lost to the region.
Thus, by mid-July there was plenty of time for the ground and vegetation to dry out, even in a normal year with full snowpack.
Want more proof for different fires?
Two other big fires were found to the east near the Columbia River: the Kailser Canyon and Molrite fires (see below), which started in mid-July
There is a nearby Snotel site at Gold Mountain (4500 ft, see map)

Below are the snowpack observations at this location (again, the black line is this year, green line indicates normal).
Way below normal snowpack! The snow melted out around April 8 rather than the normal of April 18.
Not important for a fire that would start THREE MONTHS LATER.
Still not convinced? Let's consider the largest fire, the Sinlahekin blaze near the Colville reservation in north-central Washington (see map).
There are two Snotel sites near the fire, and I will pick one of them (Salmon Meadow, 4460 ft, with the horizontal line in the map below).
This site had an abysmal snowpack, melting out on April 5, when normal is May 2. But normal melt-out was well over two months before the fire and thus the early melt-out was not relevant.
In summary, the regional snowpack melted out a week to a month early this year near the big regional fires.
But that is immaterial for wildfire because the mid-July fire initiation was over two months in the future.
Even with normal...or ABOVE NORMAL... snowpack, the melt out would have occurred two months before the fire, allowing more than enough time for the soils and fuels to dry out.
In short, the low snowpack made little positive contribution to the large fires that were initiated by lightning in July.
Finally, to provide independent evidence of this lack of connection between Washington State snowpack and fires, the plot below presents the regional snowpack on April 1 (blue line) and the subsequent fires over the region (red line).
There is little correlation between them.
Why are some folks exaggerating the role of low snowpack on regional wildfires?
Perhaps because they are trying to find a way to blame the burns on climate change, rather than invasive grasses, poor forest management, human land disturbance, and human ignitions.





Dr. Mass, you are a much needed voice of reason and much appreciated. Real science backed up by real data, what a concept.
ReplyDeleteFormer WA State Climatologist Nick Bond told me that the major impact of low snowpack is an extended fire season.
ReplyDeleteThe facts show he was in error. The previous State Climatologist Mark Albright supports the facts I have provided. Do you seen any errors in my information?
DeleteAll right. But I have a few questions.
ReplyDeleteYes, grass dries out quickly. It takes weeks to turn brown, though, as do most mountain wildflowers. (There is still a lot of green in the undergrowth at 4-5000 feet, I was hiking through some of it yesterday.) Wouldn't larger branches take longer to become really flammable? Not to mention the canopy of ponderosa pine and Douglas fir? That seems to be true of my brush pile.
Though recent rains would seem more important than spring runoff in determining that.
Snowmelt variation has a lagged effect on soil moisture through a 2-4 month window:
ReplyDeletehttps://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2013WR014541
Soil moisture and related plant hydraulic stress are strong predictors of fire spread:
https://research.fs.usda.gov/treesearch/69808
Put these together, and there's a simple story supporting the mainstream narrative: the effects of snowpack on fuel potency can linger surprisingly long after the snow's not visible on the ground. There's reams of deeper complexity pushing the case in both directions in ways situational to each fire (soil type, tree species, etc), but putting "THREE MONTHS" in all-caps isn't an automatic dunk on the mainstream story here.
Regarding forest management, Little Giant started in an moderately old burn, simmered there for several days, and when it finally took off on the next windy day, it burned right through the wide swath along Chiwawa River Road that was logged by a huge operation last year as a fire barrier. What management would have changed the story here? Prescribed burns? It started in a burn. Logging/thinning? They did it just last year.
jason...thanks. The reference you provided is consistent with what I am saying. The effects of melting snow on subsurface moisture is very small after 2 months. And, of course, surface and dead fuels dried out even more rapidly. As you note, the Little Giant fire occurred over an old burn, and looking an imagery, the area was full of dead and down vegetation...cliff
DeleteSo the fire barrier didn't work to stop the fire from spreading? It makes me question just how effective those types of fire barriers are, especially in places that get a lot of wind, as that area does.
DeleteYes, live tree foliar moisture is an important factor determining the dynamics of fire spread (particularly canopy fires), and the impact of snowpack on that metric could very well have a substantial lag.
Deletealex...I think you are missing an essential point. For two of the fires, the difference in melt-out date from normal is only about a week. Very small compared to the 2-3 months between the meltout and the fires. Could not be important..cliff
DeleteThe "snow drought" misnomer has been in play for a number of years now, despite the reality that hardly any of the state's "water resources" are fed by (hydraulically connected to) melting mountain snow (whether that be ordinary seasonal accumulation of "glacial melt"). The belief that lands across the entire state rely on mountain snow for the freshwater supply is absurd (and always has been) - a real fairy tale. I swear - there are hydrogeologists who have shied-away from speaking-up about it for fear of discommunication (integrity of the "science community" has become that bizarre, now).
ReplyDeleteI agree. I work in this realm and one cannot have a dissenting view. It’s basically ‘we can do nothing and we’re all doomed.’
DeleteThanks Cliff, as I noted in previous post the Ptarmigan fire is burning where there was above normal snowpack that did happen according to the Harts Pass snotel. Regarding moisture stress of plants, I think it is safe to say that also has less to do with moisture we receive, but amount of plants that the little moisture we get is trying to sustain. Plus, if forest canopy too thick what little moisture we get may not even reach root zones effectively. There was balance nature did, keeping forest thinned via fire.we screwed that up with supression. There is so much more than "snow drought" and "drought" and "climate change" they cite.
ReplyDeleteGood points. (Speaking of "points" - there very-very few SNOTELS (data points), not enough to make strong conclusions about diddly IMHO.) While seasonal (fall-winter) precipitation "waters" the plant cover that burns (trees, grasses, etc.), the geomorphic reality is that most of the lands on the east side of the Cascades are simply much drier than the green ocean-side western corridor. That said, more vegetation in itself doesn't necessarily drive wildfires. There isn't a chronic "wildfire season" to the west. The reality is that the vast majority of eastern Washington may correlate to snowfall stats, but I don't know at all that the soil moisture is dependent at all on "winter snow (snowmelt)". There simply isn't much [T-total] precipitation, period, east of the range.. Anyone driving through or flying over the eastern (2/3rds?) of the state recognizes that only a small minority of the terrain is green, with only a bit of that related to human activity like irrigation. The majority of the terrain (and all the flora and fauna that grows on it) survives on whatever Mother Nature dishes out. If wildfire corridors followed the path of human land-use (and I don't see that the fires do), a person might reasonably make the case that "human impacts" are much of a factor except for some types of ignition. It seems to me that planning for large fire-line zones might help protect the more densly-populated areas; but for the most part it seems to me that the natural variability of lush-dry periods will simply continue to lead to occasionally severe "wildfire seasons" and tragic events. I wonder (but don't know) what the economic benefit would pencil-out to if the state's firefighting resources (like tanker planes and devoted crews) were doubled. Those who say "the insurance industry" (meaning we - statewide premium payers) should pick up the tab when tragically big fires occur that can't be contained. That issue isn't "weather talk," but in areas where there are powerlines etc - maybe those zones should be kept completely vegetation free (tall order). As for reckless folks and arsonists...grr.
DeleteCliff - your use of the Trinity Snotel data for the Little Giant fire is dubious. The fire started up high at ~5000 feet. Trinity is at the bottom of the drainage and is ~2900’. A better comp would be the Lyman Lake Snotel site - just a few miles North of the actual fire, similarly situated East of the cascade crest and at ~5800 feet. Lyman Lake recorded the melt out date of June 13 this year, with a median date historically being July 3. I have a hard time believing that dramatic of a disparity did not play any part in fire propagation.
ReplyDeleteWhat you say is demonstrably wrong. Fire did not start around 5000 ft... satellite imager shows about 3900 ft. And then the fire spread to lower elevation. A snotel site at 5800 ft would be totally inappropriate. I am going to blog in detail about this.
DeleteWhen is Dr. mass gonna start talking to us about Frasier outflows, atmospheric, rivers, and bomb cyclones with 100 mph winds that somehow go elusive and stay 50 miles offshore teasing everybody good
ReplyDelete