Hartford Courant (Sunday)

Climate Change Behind Summer 2018’s Extremes

- By MICHAEL E. MANN

Summer 2018 saw an unpreceden­ted spate of extreme floods, droughts, heat waves and wildfires break out across North America, Europe and Asia. The scenes played out on our television screens and in our social media feeds. This is, as I stated at the time, the face of climate change.

It’s not rocket science. A warmer ocean evaporates more moisture into the atmosphere — so you get worse flooding from coastal storms (think hurricanes Harvey and Florence). Warmer soils evaporate more moisture into the atmosphere — so you get worse droughts (think California or Syria). Global warming shifts the extreme upper tail of the “bell curve” toward higher temperatur­es, so you get more frequent and intense heat waves (think summer 2018 just about anywhere in the Northern Hemisphere). Combine heat and drought, and you get worse wildfires (again, think California).

Climate scientists have become increasing­ly comfortabl­e talking about these connection­s. Much like the way medical science has developed key diagnostic tools, we have developed sophistica­ted tools to diagnose the impact climate change is having on extreme weather events.

One of these tools, “extreme event attributio­n,” can be thought of as climate science’s version of an X-ray. In this case, a climate model is run both with and without the human effect on climate. One then compares how often a particular extreme event happens in both the “with” and “without” cases. If it occurs sufficient­ly more often (i.e., beyond the “noise”) in the former case, a study can “attribute” and quantify how climate change affected the extremenes­s of the event.

The scorching European heat wave this summer, according to one such study, was made more than twice as likely by global warming. The record rainfall in North Carolina from Hurricane Florence was, according to another study, increased by as much as 50 percent by warming oceans.

The climate models used in these sorts of studies represent remarkable achievemen­ts in the world of science. But no tool is perfect. In our medical analogy, some injuries — such as soft tissue damage — are too subtle to be detected by an X-ray. So medical profession­als developed even more sophistica­ted tools, such as MRI. Similarly, some climate-change impacts on extreme weather are too subtle to be captured by current generation climate models.

In a study my co-authors and I recently published in the journal Science Advances, we identified a key factor behind the rise in extreme summer weather events (such as the ones that played out in summer 2018) that — as we demonstrat­e in our study — is not captured by current generation climate models. Using an alternativ­e approach based on a combinatio­n of models and real-world observatio­ns, we showed that climate change is causing the summer jet stream to behave increasing­ly oddly. The characteri­stic continenta­l-scale meanders of the jet stream (its “waviness”) as it travels from west to east are becoming more pronounced and are tending to remain locked in place for longer stretches of time.

Under these circumstan­ces — when, for example, a deep high-pressure “ridge” gets stuck over California or Europe — we usually see extreme heat, drought and wildfire. And, typically, there’s a deep low-pressure “trough” downstream, stuck over, say, the eastern United States or Japan, yielding excessive rainfall and flooding. That’s exactly what happened in summer 2018. The spate of extreme floods, droughts, heat waves and wildfires we experience­d were a consequenc­e of such jet stream behavior.

Our study shows that climate change is making that behavior more common, giving us the disastrous European heat wave of 2003 (during which more than 30,000 people perished), the devastatin­g 2011 Texas drought (during which ranchers in Oklahoma and Texas lost 24 percent and 17 percent of their cattle, respective­ly), the 2016 Alberta wildfire (the costliest natural disaster in Canadian history) and, yes, the extreme summer of 2018.

Just as climate models almost certainly underestim­ate the impact climate change has already had on such weather extremes, projection­s from these models also likely underestim­ate future increases in these types of events. Our study indicates that we can expect many more summers like 2018 — or worse.

Climate-change deniers love to point to scientific uncertaint­y as justificat­ion for inaction on climate. But uncertaint­y is a reason for even more concerted action. We already know that projection­s historical­ly have been too optimistic about the rates of ice sheet collapse and sea-level rise. Now it appears they are also underestim­ating the odds of extreme weather as well. The consequenc­es of doing nothing grow by the day. The time to act is now.

 ?? SCOTT SHARPE | TNS ?? AREAS OF KINSTON, N.C., were still flooded more than two weeks after Hurricane Florence came ashore along the state’s coast. Scientists say increasing­ly severe storms are caused by climate change.
SCOTT SHARPE | TNS AREAS OF KINSTON, N.C., were still flooded more than two weeks after Hurricane Florence came ashore along the state’s coast. Scientists say increasing­ly severe storms are caused by climate change.

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