After a remarkably quiet start, the U.S. tornado season exploded into action over the weekend, as a battery of tornadoes in Arkansas, Iowa, and Oklahoma killed 16 people. The Arkansas towns of Mayflower and Vilona were particularly devastated. Based on preliminary assessments, some of the twisters may have reached EF-3 or stronger on the Enhanced Fujita scale, meaning that they had wind gusts of more than 136 miles per hour.
It all amounts to quite the burst of weather whiplash. Just days ago, after all, USA Today could be found calling 2014 the "safest start to tornado season in a century." April 2014 was certainly looking nothing like April 2011, which featured a staggering 753 tornadoes in the United States, a new all-time record. So what's up with this sharp variation in the behavior of tornadoes, these extraordinarily powerful storms that afflict the U.S. more than any other part of the world? And could global warming have something to do with the matter?
Until pretty recently, scientists really felt that they couldn't say much about that question. "The issue of global warming and severe thunderstorms [which often result in tornadoes] has been an outstanding challenge for the scientific community," explains Noah Diffenbaugh, an Earth scientist at Stanford University who has focused on the question. For instance, a recent consensus report on extreme storms and climate change, published early last year in the Bulletin of the American Meteorological Society, found that there was "little confidence" of any trend in tornado occurrence, and also concluded that there were no clear changes in the environments in which these storms form.
Tornadoes emerge in some, but not all, severe thunderstorms, powerful explosions of atmospheric energy that also frequently feature lightning, hail, strong winds, and intense rainfall. Scientific research has determined that while a variety of environmental and atmospheric conditions support severe thunderstorm development, two in particular are crucial. The first is that there have to be high levels of so-called "convective available potential energy," or CAPE, which denotes the instability of the atmosphere, and thus how friendly it is to thunderstorm updrafts. The second condition is that there must be strong wind shear, defined as the difference in speed or direction of winds as one ascends from the surface higher into the atmosphere.
Based on this knowledge, researchers have turned to global climate models in order to predict how global warming could change the relationship between CAPE and shear in the the future. And for a long time, the two factors were basically expected to offset each other. Or as National Oceanic and Atmospheric Administration tornado researcher Harold Brooks put it in a 2013 paper summarizing the consensus: "Climate model simulations suggest that CAPE will increase in the future and the wind shear will decrease." So even though higher overall heat might lead to the potential for more explosive storms, the expected decrease in shear meant that potential might not get realized. In other words, it was basically looking like a wash.
That means more favorable environments for severe thunderstorms in general, but what about the subset of those storms that produce tornadoes? For tornado occurrence, Diffenbaugh explains, wind shear very close to the surface appears to be particularly important. In their new modeling study, Diffenbaugh and his colleagues looked at this parameter too, and they found an "increase in the fraction of severe thunderstorm environments that have high CAPE and high low-level shear," as Diffenbaugh puts it. As the authors wrote, this result is suggestive "of a possible increase in the number of days supportive of tornadic storms."
The paper by Diffenbaugh and his colleagues represents "the first significant evidence that we might expect to see a change in tornadoes," says NOAA's Brooks.
Meanwhile, Brooks thinks he might have found a trend in a different area: actual tornado statistics. In general, the scientific consensus has been that our tornado data just isn't good enough to support the idea of any clear, historic trend in tornadic activity. But in his latest research, Brooks thinks he has detected a "pretty strong signal that there's been an increase in the variability of tornado occurrence on a national scale." What does that mean? Basically, an increase in erratic behavior: periods with little or no activity, followed by intense bursts of activity.
There's been "a decrease over the last 40 years in the number of days per year with at least one F1 tornado occurring somewhere in the US," says Brooks. "At the same time, there has been an increase in the number of days with at least 30 F1 tornadoes."
As noted above, recent tornado behavior has certainly seemed pretty up and down. According to Brooks, in recent years we've seen records for the most tornadoes ever in a 12-month period, as well as for the fewest in a 12-month period. And Brooks says we are also seeing increasing variability in terms of when the tornado season actually starts. (Note: The relationship between Diffenbaugh's research, and Brooks' new finding, isn't clear at this point.)
In summary, then, it would be very premature to say that scientists know precisely what will happen to tornadoes as global warming progresses. However, they have come up with some interesting new results, which point to potentially alarming changes. More generally, the upshot of this research is that tornadoes must change as a result of climate change, because the environments in which they form are changing.