Since the invention of weather radar, anecdotes have swirled about how a thunderstorm changes as it approaches and moves across a city. The stories involve a storm suddenly splitting and reforming downwind of a city or, in a related way, suggest that a thunderstorm is producing more rain immediately downwind of a city.

These concepts have long been a source of interest to people studying mesoscale meteorology, which covers weather systems that are between a few miles to several dozen miles in size. These include sea breezes, tropical rain bands and thunderstorm complexes.

The Atlanta skyline is seen as thunderstorms move through July 24, 2017. Two scientists used Atlanta as their prototype city when studying the impact of urban areas on thunderstorms.

Gathering data to understand the behavior of storms at the mesoscale level has historically been challenging. For many years, the surface observation network, radars and satellite imagery were all too coarse to catch those smaller scale wind patterns and circulations.

But observation technologies are getting better, and computers are getting faster, allowing the scientific community to investigate these weather phenomena more closely. Using those tools at the University of Georgia, Marshall Shepherd and Jordan McLeod are among those looking for answers.

McLeod

Cities are hotter than the surrounding rural and suburban areas, as energy from the sun heats up asphalt, concrete and bricks much more than the trees, grasses and vegetation in those surrounding areas. As a result, a small-scale heat dome can develop over a city during the day, extending up to a mile above the ground. The localized hot spot affects wind patterns within a city and between the city and its surrounding areas.

Applying that understanding to their investigation, they found a particular set of circumstances that occasionally enhances summertime thunderstorm rainfall immediately downwind of a city: weak westerly winds about 10,000 feet above the ground, unusually humid air through a deep level of the atmosphere, and ground-level winds that are slightly converging. This enhancement is known as the urban rainfall effect.

The effect is not a dominant one, but it is perceptible. Using Atlanta as their prototype city, their analyses indicate that the urban rainfall effect is detectable in about 8 percent of the summer days they studied.

McLeod, now a meteorology instructor at the University of South Alabama, has done some preliminary studies around other large cities in the Southeast.

“We noticed a similar footprint, over and downwind of the metropolitan areas — an enhancement of convective rainfall during the summer season,” McLeod said.

For now, it appears that the impact is generally confined to the summer, when there are not many other large scale atmospheric motions to drive the weather.

“It kind of operates in the background. It’s not an overwhelming signal on most days — it kind of sneaks up on you,” McLeod said.

People sit out a thunderstorm before a baseball game between the Atlanta Braves and the Arizona Diamondbacks on July 30, 2022, in Atlanta.

The additional amount of rain from the urban rainfall effect is still difficult to quantify precisely, as the variability in the data signal is small. Nonetheless, it is significant and large enough to measure.

In addition to enhancing the rainfall downwind of storms, these conditions can also lead to thunderstorms originating right over a city or, in some cases, modify a storm as it approaches a city. There is increasing evidence that a storm can split — or at least weaken — as it approaches a city, although the precise reason why requires much more study.

“Sometimes, if the conditions are just right, a storm will split around the city and reform downwind. That’s another way we see amplifications of rainfall downwind of a city,” McLeod said.

Sean Sublette is the chief meteorologist for the Richmond Times-Dispatch in Virginia.


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