Friday, December 17, 2021

The Making of a Historic Wind and Fire Event

The recent historic wind and fire event that literally blew through the Great Plains was anomalous in every sense of the word. But, not all anomalies are created equal. We see high-impact events all the time, but not all fall into the historic category. With today’s post I wanted to dig into some of the science behind this event and what set it apart from other high-end events.

Let’s first set the stage. A potent shortwave ejected out of the Central Rockies Wednesday morning, December 15, 2021, and very rapidly lifted northeast from the Central Plains into the Upper Midwest/Great Lakes by Wednesday night. Negatively-tilted shortwaves often mean business, and this one was no different.

What set this system apart from similarly-tilted shortwaves was the very strong mid-level jet that accompanied it. The observed 12z sounding at ABQ showed a 500mb wind speed of 100kt, while the observed 12z DDC sounding measured a 700mb wind of 65 kt. 


The 21z RAP 500mb analysis (shown earlier) suggested a peak mid-level wind speed of around 120 kt at 500mb as it moved out over Kansas. A mid-level jet that strong this time of year is more unusual.

Let me pause here a minute. Take a close look at that DDC sounding again. 


 On a day like this, with deep mixing expected, you can sometimes use an observed morning sounding to get a rough idea of how strong the winds might be in that area later in the day. In this case, the morning started with a fairly stout inversion across western and central Kansas, but the forecasted combination of daytime heating with cooling aloft (beneath the shortwave) suggested the potential to mix deeply, with the sounding revealing how strong the winds may be within that mixed layer. The DDC sounding, for example, showed 60-80kt in the potential mixed layer, suggesting peak wind potential of 80-90 mph for any area that could mix deep enough. The 21z RAP analysis reveals the areas from western to central Kansas where some of the deepest mixing occurred (shown by the steepest low-level lapse rates).

At the surface, an unusually deep surface low developed, adding a strong pressure gradient component to the wind potential. In Minnesota, the low pressure set arecord. The strong downslope drying east of the Rockies also helped setup a sharp dryline across Nebraska and Kansas.


 

The ECMWF’s Extreme Forecast Index (EFI) really helps put it all together. The EFI is a great forecasting tool to help determine which events may be anomalous. It can also reveal the anomalous events that are not like the others. 

On the map above, you’ll notice the EFI is maxed out (pink shading) over a large area of the Plains. Looking closer, though, you’ll notice a Shift of Tails (SoT) of 2. In my experience, that’s a separating marker between events. For wind, the combination of a high EFI value AND a SoT of 2 puts an area in a higher-end, potentially record-breaking, setup. The end result? A widespread area of verystrong, damaging winds. The wind, alone, was anomalous, but this event didn’t stop there.

When you overlap strong winds with a warm and very dry airmass, bad things tend to happen. This event appeared to be a classic fire outbreak setup, as researched and shown by Lindley,et al.

 

Adding fuel to the fire, literally, was very dry antecedent conditions. From an anomaly standpoint, there was a very large footprint of dry conditions across Kansas, with much of the state running 10-25%, or less, of normal for rainfall (since November 1, 2021). Fire weather aside, this also added to the risk of blowing dust.

 

Higher end fire weather days do occur on the Plains, but another aspect of this event that sets it apart is that it came in December. This December has been an active one for fire weather in Kansas. In fact, since 2006, only one other December was more active (2017). Outside of 2017, no other December in that time period even comes close.


Lastly, I want to highlight the anomalous combination of shear and instability, by December’s standards. The focus for severe weather was over the Upper Midwest, but it all started in the Central Plains. A plume of high PWats surged north through the Central Plains, ahead of the ejecting shortwave, and went well north all the way into, and through, the Great Lakes region. Getting that amount of moisture return that far north in December is a low frequency occurrence, and more unusual in December.


 
A moistening airmass beneath steep lapse rates and cooling temps aloft supported modest destabilization, and a weakening cap, ahead of the advancing dryline/Pacific cold front. This was accompanied by more than adequate shear for organized severe convection.



The shear/instability combo isn’t unusual for this part of the U.S., in general. In December, though? Not so much. An anomalous combination of shear and instability stretched from Kansas to Michigan, setting the stage for a remarkable swath of severe weather, including several tornadoes. And notice, once again, a Shift of Tails of 2 on the EFI plots below.

For perspective, Kansas, Nebraska, Iowa, and Minnesota have had more Severe Thunderstorm Warnings issued this December than any other December on record (dating back to at least 1986, based on IEM data). Since this post was focused on the science and anomalies of the event, though, I’ll leave the product climatology for another day. 

In summary, a truly historic, mid-latitude storm system had a “perfect storm” combination of high-end anomalies from top to bottom, and everywhere in between. Anomalous features regularly come around, but not all at the same time. Every now and then, though, they line up in perfect sync, often with devastating impacts. This post only touches the surface of the science involved in this event, but I hope it provided a little context to just how anomalous and unusual this event was over a huge footprint of the U.S., while also serving as a mini training moment for what to look out for in future higher-end wind and fire events. 

NOTE: Some of the mesoanalysis images shown above were from the NWS Wichita’s event summary. I helped make that summary, and the images I used in this blog are ones I made. I just wanted to clarify that in full disclosure to make sure it is understood that those images were not improperly taken from someone else's work.