The effect of urbanisation on temperature is relatively well known – cities are often measurably warmer than their surrounding rural areas. This is called the urban heat island effect.
What fewer people know is that the urban heat island has a twin counterpart with similarly important consequences: the urban precipitation anomaly, where the presence of urban development measurably affects the amount of rainfall in an area.
In a new study published in Proceedings of the National Academy of Sciences, researchers at The University of Texas at Austin looked for evidence of precipitation anomalies in 1,056 cities across the globe and found that more than 60 per cent of those cities receive more precipitation than their surrounding rural areas.
In some cases, the difference can be significant. For instance, researchers found that Houston, on average, will receive almost 5 inches more rain per year than its surrounding rural areas.
This could have wide-ranging implications, the most serious of which is worsened flash flooding in densely built urban areas.
Variation in urban rainfall is something scientists have known about for several decades, but never at a global scale.
Study author, Xinxin Sui, a doctoral student at the Cockrell School of Engineering, said, “Previous studies looked at only certain cities and storm cases.” For this paper, she and other researchers pored over precipitation data sets from satellites and radar systems, examining daily precipitation anomalies for these 1,056 cities from 2001 to 2020.
Sui said, “In general, we found that over 60 per cent of these global cities have more rainfall than the surrounding countryside. Then we compared with different climate zones and found that if the local climate is hotter, if it’s wetter, then it may have a larger rainfall anomaly compared to the cities in cooler and dryer places.”
In addition to Houston, the list of large cities with the largest precipitation anomalies includes Ho Chi Minh, Vietnam; Kuala Lumpur, Malaysia; Lagos, Nigeria; and the Miami-Fort Lauderdale-West Palm Beach metropolitan area.
Study author Dev Niyogi, a professor at both the Jackson School of Geosciences and Cockrell School of Engineering, explained that urban areas tend to take rain from one location and concentrate it in another, much like a sponge that is being squeezed.
“If you were to pinch one part of the sponge, you would have water coming down more forcefully from one side,” he said. “The amount of water you have in the sponge is the same, but because now you have that dynamic sort of squeezing the atmosphere, you have more ability to take the water out from that location.”
Roberta Boscolo is the Climate & Energy Leader at World Meteorological Organisation and was not involved in the study. She said, “The implications are vast, with urban planning and infrastructure needing to adapt to growing challenges like flooding. The research underlines the importance of integrating weather and climate considerations into urban design for sustainable future cities.”
Although it’s less common, some urban areas actually receive less rainfall than their surrounding rural counterparts. This typically occurs in cities situated in valleys and lowlands, where precipitation patterns are controlled by nearby mountains. The cities where this is most pronounced include Seattle, Washington; Kyoto, Japan; and Jakarta, Indonesia.
There are several reasons why most cities receive more rainfall than their rural neighbours. Co-author Zong-Liang Yang, professor at the Jackson School, said one key factor is the presence of tall buildings, which block or slow wind speeds. This leads to a convergence of air toward the city center.
Yang said, “The buildings further enhance this convergence by slowing the winds, resulting in a stronger upward motion of air. This upward motion promotes the condensation of water vapor and cloud formation, which are critical conditions for producing rainfall and precipitation.”
Researchers found that population has the largest correlation with urban precipitation anomalies compared with other environmental and urbanisation factors. This is because larger populations typically create denser and taller urban areas, along with more greenhouse gas emissions and, therefore, more pronounced heat.
This phenomenon has implications for all cities heading into a future of climate change, said Yang, who described how the increased chances of rainfall in cities combined with the impervious surfaces that make up their urban environments can be a recipe for flash flooding.
Read the research, Global scale assessment of urban precipitation anomalies