A warming climate will increase the number of tropical cyclones and their intensity in the North Atlantic, potentially creating more and stronger hurricanes, according to simulations using a high-resolution, global climate model.
“Unfortunately, it’s not great news for people living in coastal regions,” says Christina Patricola, an Iowa State University assistant professor of geological and atmospheric sciences, an affiliate of the US Department of Energy’s Lawrence Berkeley National Laboratory in California, and a study leader.
“Atlantic hurricane seasons will become even more active in the future, and hurricanes will be even more intense,” Patricola says.
The researchers ran climate simulations using the Department of Energy’s Energy Exascale Earth System Model and found that tropical cyclone frequency could increase 66% during active North Atlantic hurricane seasons by the end of this century.
Those seasons are typically characterized by La Niña conditions—unusually cool surface water in the eastern tropical Pacific Ocean—and the positive phase of the Atlantic Meridional Mode—warmer surface temperatures in the northern tropical Atlantic Ocean.
The projected numbers of tropical cyclones could increase by 34% during inactive North Atlantic hurricane seasons. Inactive seasons generally occur during El Niño conditions with warmer surface temperatures in the eastern tropical Pacific Ocean and the negative phase of the Atlantic Meridional Mode with cooler surface temperatures in the northern tropical Atlantic Ocean.
In addition, the simulations project an increase in storm intensity during the active and inactive storm seasons.
“Altogether, the co-occurring increase in (tropical cyclone) number and strength may lead to increased risk to the continental North Atlantic in the future climate,” the researchers write.
Patricola adds: “Anything that can be done to curb greenhouse gas emissions could be helpful to reduce this risk.”
What are North Atlantic tropical cyclones? “Tropical cyclone is a more generic term than hurricane,” Patricola says. “Hurricanes are relatively strong tropical cyclones.”
Exactly, says the National Oceanic and Atmospheric Administration. Tropical cyclone is a general reference to a low-pressure system that forms over tropical waters with thunderstorms near the center of its closed, cyclonic winds. When those rotating winds exceed 39 MPH, the system becomes a named tropical storm. At 74-plus MPH, it becomes a hurricane in the Atlantic and East Pacific oceans, a typhoon in the northern West Pacific.
Patricola and another group of collaborators have also published a second research paper about tropical cyclones, also in Geophysical Research Letters. The paper examines a possible explanation for the relatively constant number of tropical cyclones observed globally from year to year.
Could it be that African Easterly Waves, low pressure systems over the Sahel region of North Africa that take moist tropical winds and raise them up into thunderclouds, are a key to that steady production of storms?
Using regional model simulations, the researchers were able to filter out the African Easterly Waves and see what happened.
As it turned out, the simulations didn’t change the seasonal number of Atlantic tropical cyclones. But, tropical cyclones were stronger, peak formation of the storms shifted from September to August, and the formation region shifted from the coast of North Africa to the Gulf of Mexico.
So African Easterly Waves many not help researchers predict the number of Atlantic tropical cyclones every year, but they do appear to affect important storm characteristics, including intensity and possibly where they make landfall.
Both papers call for more study.
“We are,” Patricola says, “chipping away at the problem of predicting the number of tropical cyclones.”
Source: Iowa State University
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