My group and scientists from the University of Albany are now studying the meteorology of the LA wildfires earlier this month and have significant early results. At the American Meteorological Society meeting last week, I attended many wildfire meteorology sessions and talked to several colleagues who have actively studied such events. The LA fires were a topic of considerable discussion.
We have a good idea of what happened: an extreme/unusual Santa Ana event associated with severe downslope winds. In this blog, I will show you some early simulations and explain why this event occurred.
I will also describe why climate change did not play a significant role.
As I will explain below, this is not only a Santa Ana event, but an unusual one, with extreme winds descending to lower elevations. Some lower-elevation stations, such as Burbank, experienced their strongest wind gusts on record. Model simulations suggest the development of what is known as a high-amplitude mountain wave leading to a downslope windstorm event.
Santa Ana 101
Santa Ana's are associated with strong northeasterly (from the north to east) winds over southern California. These strong winds are accompanied by very low relative humidity and are very favorable for southern CA wildfires.
The typical large-scale weather pattern associated with Santa Anas includes a large high-pressure area over the Great Basin, with the strongest events also having a low center to the southwest (see below). Such a pattern results in strong northeasterly winds approaching the mountains of southern CA.
The observed sea level pressure pattern at 4 PM January 7 (below) showed many of these elements, with the low to the south being particularly strong (warm colors indicate above-normal pressure, cool colors show below-normal pressures).
This pattern produced extreme, perhaps precedented. northeasterly winds approaching the region in the lower atmosphere. To illustrate, the color shading in the map below shows wind differences from normal at 925 hPa (about 2500 ft above sea level) at 10 PM Tuesday (January 7) evening. The light gray indicates very unusual winds (more than six standard deviations from normal). The wind direction and speed at some points are also shown.
This was not your normal Santa Ana.
High-Resolution Simulations
To understand what happened, UW Research Scientist David Ovens, a member of my research group, ran a very high-resolution forecast/simulation of the event using the WRF model, with a grid spacing of 1.3 km (this is very high resolution).
Let me show you a surface wind gust forecast (32 hours into the prediction) for 12 AM on Wednesday, January 8. The areas of the Palisade and Eaton fires (the two biggest ones) are shown by red outlines.
Extreme winds (with gusts exceeding 70 knots, 81 mph) were forecast over and downwind of the San Gabriel Mountains. HUGE threat. Lesser, but still strong winds (50-60 mph gusts) are noted in the Palisades area extending to the west and south.
To understand what is going on, it is useful to plot vertical cross-sections through the fire areas to show the 3-D atmospheric structure. Below is a cross-section (at 8 PM Tuesday) through the Eaton fire; a section that crosses the San Gabriel Mountains. The shading shows sustained winds in knots, the x-axis is the horizontal distance and the y-axis is height in pressure (700 is about 10,000 ft)
Wow. Very strong acceleration of the air as it descends the southern slopes of the San Gabriels, with the strongest winds near Altadena, where the fire went crazy. This was a very powerful downslope windstorm with a highly amplified mountain wave pattern.
Another cross section, this time going through the Palisades fire at 10 AM on Wed. January 8, is shown below. Very strong winds to the lee (south) of both the interior mountains and Santa Monica mountains to the south (left side of the figure).
These and earlier simulations by the UW WRF model and NOAA/NWS models (such as the HRRR, High Resolution Rapid Refresh) consistently forecast the extreme downslope winds DAYS in advance.
It was also clear that there were unusually large amounts of dried "fuels" ready to burn. The fuel load was particularly high after TWO unusually wet winters (2022-2023, 2023-2024). A dry start of winter ensured massive amounts of fuels were ready to burn.
This was clearly a situation of extraordinary extreme wildfire danger. That is why I blogged a strong warning the day before. Why the National Weather Service did the same. LA officials should have know a severe threat was in place.
All that was needed was an ignition source. For the deadly and large Eaton Fire near Pasadena, it appears that a problematic electrical transmission tower was the origin of the fire.
For the Palisades inferno, it is either some smoldering embers from a New Year's Eve fireworks blaze or the failure of some aged powerlines found north of Skull Rock. Perhaps, arson is another possibility. Several fire experts I talked to at the AMS wildfire meeting thought the powerlines were the most probable cause, but a definitive evaluation is not yet available.
What is clear is that LA did not shut off the power to the region even AFTER the fire was initiated and that only limited fire-fighting resources were in place before the fires began. Not good.
Bottom Line: A very skillfully predicted Santa Ana event with record-breaking winds hit LA earlier this month. Two wet winters resulted in unusually high levels of dried fuels. Human ignitions initiated the fires.
Influence of Global Warming
There are several media outlets and climate activists that are suggesting that LA fires were the result of global warming or significantly enhanced by human-caused warming.
These claims are contrary to the best science, which indicates minimal impacts of human-caused warming.
Such claims undermine the importance of key societal failures, from not shutting off power and fire-hardening homes to not having sufficient fire-fighting capabilities or adequate warnings and evacuation protocols.
Key reasons why global warming is not an important factor include:
1. There is no evidence that global warming increases Santa Ana winds. In fact, there are strong physical reasons (with supporting scientific literature) that global warming WEAKENS Santa Ana winds.
2. The available fuels were unusually abundant because the two previous years have been much wetter than normal. There is no evidence this is caused by global warming. And there is no long-term trend for wetter winters, which would be evident if this was a climate issue.
3. The immediately prior months were drier than normal. This is not predicted by global warming projections and there is no historical trend to drier early winters which would occur if climate was a cause (see plot below of Los Angeles precipitation for Oct. 1-January 6 ).
3. There are some outrageous claims that the LA fires are the result of increasing "weather whiplash" due to climate change. This "whiplash" theory is unsupported by observations, such as the plot shown above.
I am particularly troubled by the media pushing weather/climate theories that are untrue. A prime example is the unsupported claim that the Lahaina fire was associated with the passage of a hurricane to the south. This was proven to be false.
You said a couple of weeks ago that the jet stream shift to the south could bring precipitation to Southern California. Didn't happen. Do you see any precipitation for that region in the near future?
ReplyDeleteOne other tool used to get an idea of the strength of offshore winds, are by looking at designated surface pressure gradients. LAX-DAG gradient is a good indicator of NE-SW direction. (Typical Santa Ana wind direction). During the initial afternoon through evening on Jan 7th. The LAX-DAG gradient was not very In fact the LAX-BFL gradient (N-S direction) was a few mb stronger. The placement of the upper low over Baja/ AZ had a lot to do with energizing this damaging Santa Ana. Cliff mentioned all of the reasons and showed the graphs to back it up. My 2 cents is. Typical LAX-DAG gradient winds ( not including strong upper support) affects the I-5 corridor including Castaic below the Tejon Pass, Santa Clarita, Central and eastern San Fernando Valley including Sylmar, Burbank. Van Nuys, and through the Sepulveda Pass and Hollywood Hills to Santa Monica and Pacific Palisads. The typical NE Santa Ana wind direction generally affects the mountains of LA and Ventura Counties into The I-14 corridor into Acton, Canyon Country. Also Santa Clarita, western San FernandoValley, much of Ventura County to the coastal plain. Also the Santa Monica Mtns usually Malibu and areas west. (Lighter breezes for Pacific Palisades). Also the passes and canyons in the San Gabriel Valley including Eaton Cyn. If upper support is strong. Then mountain wave activity can bring surfacing damaging winds across the 210 and 118 corridors. I've worked many of these strong Santa Ana and I-5 corridor events. Relatively cold events drive stronger events, and mountain waves can bring more damaging winds to areas not usually affected. Nice write up Cliff!
ReplyDeleteThanks....as you note, SL pressure gradients are better for gaps in mountain ranges than when mountain waves are critical (as in this event)..cliff
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