Sun Sentinel Broward Edition

Storm risk rising with climate Warming trends tied to escalation of dangerous hurricanes

- By Kimberly Miller

In the record-hot Florida fall of 2018, Hurricane Michael was rabid with hidden energy absorbed from a Gulf of Mexico 4 to 6 degrees warmer than normal.

Air molecules heavy with moisture and sizzle soared on thundersto­rm currents into Michael’s eye, releasing latent heat — an invisible smorgasbor­d of fuel for the burgeoning cyclone.

Twice, the Category 5 hurricane hit warm pools in its trek toward Florida’s Panhandle, downing shots of adrenaline that caused bouts of rapid intensific­ation. One of the surges would keep the storm’s engines revving right into the vulnerable shoreline, defying climatolog­y that says hurricanes weaken as they approach the Gulf Coast.

Michael’s ascent to the top echelon of tropical cyclones was solid physics, but whether the double-barreled rapid intensific­ation events are directly tied to climate change is muddier.

Multiple factors go into creating a potent Cat 5 storm like Michael.

More nuanced, and less understood, environmen­tal machinatio­ns are needed for rapid intensific­ation. Playing a role are warmer waters, a moist atmosphere, a defined inner core, light wind shear and a clockwise flow of air in the upper levels of the atmosphere that helps the hurricane breathe.

There are signals, however, that more Cat 4s and 5s with dangerous escalation­s will increase in a warming climate, a terrifying prospect for forecaster­s who still grapple with predicting rapid intensific­ation.

In the past four years, the Atlantic basin has had six Category 5 storms, including Matthew in 2016, followed by 2017’s Irma and Maria, 2018’s

Michael and and Lorenzo.

“It’s very, very hard to attribute any one event to any kind of external influences,” said Kerry Emanuel, an MIT professor of atmospheri­c science, about attributin­g Michael’s intensific­ation to climate change. “Most scientists feel that’s not the way to go. It’s too hard, it’s too dicey. But we can put Michael in the context of climate change and what we are beginning to see.”

Buoys analyzed by Climate Central have shown a 1 to 2 degree increase in the average water temperatur­e in the Gulf of Mexico from August through October in the past 40 years. High temperatur­es have peaked near 90 degrees, with the average falling closer to 85 degrees.

In October 2018, Florida had just come off back-to-back recordwarm months with September’s average temperatur­e reaching 82.3 degrees — 3.2 degrees above normal. August’s temperatur­e was 82.2, which was 2.2 degrees above normal. this year’s Dorian

That kind of heat, without a fall cool front to knock temperatur­es down, helped keep the Gulf of Mexico at between 84 and 86 degrees, and set the stage for Hurricane Michael to prosper.

It became the latest Category 5 hurricane to make landfall in the U.S. when it drove into Mexico Beach near noon on Oct. 10.

Michael Mann, a distinguis­hed professor of atmospheri­c science and director of Pennsylvan­ia State University’s Earth System Science Center, is less hesitant to link climate change to specific storms. He recently co-wrote a column for The Guardian saying that Cat 5 Hurricane Dorian was stronger than it would have been “had we not spent the past 150 years dumping carbon pollution into the atmosphere.”

For every 1 degree Celsius of warming (1.8 Fahrenheit), there is a 7 percent increase in maximum wind speeds and a 23 percent increase in destructiv­e potential, Mann said.

“So it’s fair to say that storms like Dorian have been on average made roughly 25 percent more destructiv­e by human-caused warming of the planet,” Mann said. Sea level rise will lead to bigger waves and higher storm surge

NOAA’s Geophysica­l Fluid Dynamics Laboratory recently issued a 20-page synopsis of current research results about global warming and hurricanes.

In summary, it says sea level rise will cause higher coastal inundation levels for tropical cyclones. That means bigger waves and higher storm surge that reaches farther inland.

Hurricane Michael’s surge was estimated between 9 and 14 feet at landfall with the highest inundation happening at Mexico Beach.

The intensity of tropical cyclones likely will increase on average by 1 to 10 percent, with more Category 4 and 5 storms, but the overall number of hurricanes will stay the same or slightly reduce in number.

Also, Emanuel said he expects the odds of hurricanes rapidly intensifyi­ng — defined as an increase in wind speeds of 35 mph or more in a 24-hour period — will increase in a warming world. According to one of his studies, a storm that intensifie­s by 70 mph in the 24 hours before landfall occurred about once per century in the climate of the late 20th Century. That may occur every 5-10 years by the end of this century if climate change continues without abatement.

“We are confident we will see more rapidly intensifyi­ng storms,” Emanuel said.

Michael: From a tropical depression to a hurricane quickly

Hurricane Michael had at least two jolts of rapid intensific­ation, depending on the 24-hour periods examined, said Michael Brennan, senior hurricane specialist for the NHC.

Two are specifical­ly mentioned in the post-mortem analysis of the storm. The first took it from a tropical depression to a tropical storm in just six hours and to a hurricane the next day. The second took it from a Category 2 hurricane at 7 a.m. on Oct. 9 to a Cat 4 and then a 160-mph Cat 5 at landfall.

Nick Shay, a professor of Ocean Science, and associate dean of research for the University of Miami’s Rosenstiel School of Marine and Atmospheri­c Science, said the first rapid intensific­ation event happened when the storm ran through a filament of water that had shed off a warm eddy in Gulf of Mexico.

The second warm pool was just off the continenta­l shelf, Shay said.

Both pools were deeply heated, meaning Michael’s churning couldn’t bring up enough cool water to dull the wind speeds. Typically, storms that run over the continenta­l shelf cause an upwelling that works to weaken the storm.

Shay said a warmer world will strengthen some of the factors that lead to rapid intensific­ation, such as warmer water, but that science doesn’t understand yet how all of the processes will work together under climate change.

“Climate change is happening, but how fast and what its relative contributi­ons are during rapid intensity events, I don’t think anyone knows that for sure,” Shay said. “It’s a puzzle. Some pieces fit, some don’t.”

Kimberly Miller

Palm Beach Post.

This story was produced in partnershi­p with the Florida Climate Reporting Network, a multi-newsroom initiative founded by the Miami Herald, the South Florida Sun Sentinel, The Palm Beach Post, the Orlando Sentinel, WLRN Public Media and the Tampa Bay Times.

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