Lightning has been widespread over Alaska in the past several days, and wildfires have sprung up as an inevitable consequence. According to the latest information on akfireinfo.com, fires have burned about 25,000 acres statewide so far this season, which is about normal for the time of year. Fire activity typically ramps up quickly in June, with burn acreage often exceeding 200,000 acres by the end of the month.
Year-to-year variability of fire acreage in Alaska is a very interesting topic and a fascinating and challenging prediction problem. I'd like to do an in-depth study of it one day, but today I'll just make a couple of points. First, consider the map below, showing a 23-year correlation between sea surface temperatures in May and the subsequent fire acreage rank. I've used the rank of the fire acreage (with higher rank for higher acreage) rather than actual acreage numbers because the distribution is strongly non-Gaussian.
There is a better correlation (+0.44) between Alaska fire acreage and the North Pacific Mode (NPM) index. The NPM pattern is focused between 40 and 50°N across the North Pacific, and according to the first map above, this is an area that shows some connection with Alaska fire activity.
So what do current conditions look like? The map below shows the May analysis; the NPM was slightly positive, as it has been for the last 4 months, but it's not a dramatic anomaly (excepting the Bering Sea warmth). This suggests that ocean temperature patterns are only slightly favorable for enhanced fire activity this year. As an aside, there seems to be no sign of the strongly positive NPM phase that the long-range models were predicting earlier in the year (and are still predicting).
We can also search for fire-acreage-related precursor patterns in the atmosphere. According to the map below, there is a statistically significant - but not highly robust - correlation between 500mb heights over Alaska in May and subsequent fire acreage. This makes sense; if the weather pattern sets up with a ridge over Alaska during May, then dry and sunny conditions will reduce fuel moisture, and the next month or two are also more likely than not to be warm and dry.
How about May 2018? Rather than having a ridge over the state, there was a trough over the southwest, and most of the interior was wetter than normal. So this points to reduced fire activity, albeit with low confidence.
And now perhaps the most interesting result that I've stumbled upon in this brief analysis. The map below shows the average SST anomaly in winters following the 6 most active fire seasons since 1995. Most readers will recognize the pattern immediately: the warm band along the equator in the central and eastern Pacific is a classic El Niño pattern. This suggests that very active fire seasons in Alaska have a strong tendency to be followed by significant El Niño episodes.
The last point to make is that the latest data from the long-range computer models have recently shifted quite decisively in favor of El Niño for the coming winter (2018-19); so it will be most interesting indeed to see how the rest of the fire season evolves in Alaska.
This may have been discussed previously, but lightning = naturally occurring/non-human induced fires. This year in Fairbanks (and maybe over Alaska in general?) we've had some vigorous daily thunderstorms and associated lightning.ReplyDelete
Certainly more so far this season than some years I recall. So how about another look at the number of lightning strikes and the conditions you note in the Pacific Ocean?
Fires are of course a consequence but maybe not a primary component. Analyzing strikes vs resulting fire acreage would be informative. Maybe it's already been done.
With Gary's comment I was starting to think about other proxies to fire acreage. Fires are a subset of lightning caused by thunderstorms. There isn't many dry thunderstorms in the Interior. Weather reports have described thunderstorms for the longest time. And thunderstorm rain totals can be distinguished from other rain by hourly behavior. So we have some proxies for acreage extending well beyond a couple decades. This would allow one to determine the relationship between ENSO and Alaskan fires throughout Alaskan history, possibly strengthening the relationship you have found.ReplyDelete
I'll also point out an observation. It seems that we are more likely to get thunderstorms when the flow is from the East.
Thanks to both. It certainly would be interesting to look at lightning itself, i.e. how well it correlates to both fire acreage and large-scale weather patterns. I have only passing familiarity with the historical lightning database but will see if I can dig into it.ReplyDelete
My comments weren't meant to diminish or confuse your analysis Richard nor create extra work. If estimates of burned acreage precede lightning detection, and correlate well with recent estimates of both (see analysis links below), then maybe either database will be a suitable proxy for analysis.Delete
But perhaps even precursors of thunderstorms and their resultant lightning would be better. For example seasonal temps, moisture, lifting indices, and heights (or what best creates the conditions).
A clouding issue (pun) might be human caused fire acreage instead natural occurrences. Also a factor in ultimate acreage are fires that once started were allowed to burn versus those quickly extinguished.
Maybe simple fire starts exclusive of acreage would be better? Using starts gets rid of the results biased towards ground conditions suitable for fire expansion, but may ignore the acreage that later develops due to upper air conditions mentioned in the analysis above.
Lightning strike detection is a newer tool and one that undergone changes to sensor range and location.
Here's some info and data links for lightning:
And some previous analysis:
Enough damage for now.
Better link for #3 analysis above:Delete