{"id":52583,"date":"2026-08-24T15:47:10","date_gmt":"2026-08-24T20:47:10","guid":{"rendered":"https:\/\/nelson.wisc.edu\/the-commons\/?p=52583"},"modified":"2026-08-24T15:47:11","modified_gmt":"2026-08-24T20:47:11","slug":"taking-the-citys-temperature","status":"publish","type":"post","link":"https:\/\/nelson.wisc.edu\/the-commons\/taking-the-citys-temperature\/","title":{"rendered":"Taking the City’s Temperature"},"content":{"rendered":"\n

On some days, Madison’s streets and buildings trap enough heat to make the city noticeably warmer than the surrounding countryside. On others, the opposite occurs. New research co-authored by Elizabeth Berg and Christopher Kucharik explores the weather conditions behind these shifting patterns and offers new insights for urban climate planning.<\/p>\n\n\n\n

Published in City and Environment Interactions<\/em>, the study<\/a> analyzed 12 years of data from an extensive network of temperature sensors to better understand how weather, seasonal patterns, and longer-term climate variability influence the temperature differences between the city and its surrounding rural areas. Rather than treating the urban heat island as a static phenomenon, the researchers found that its intensity shifts considerably depending on environmental conditions.<\/p>\n\n\n\n

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Illustrating eight land use types, shown with the corresponding relative temperatures. Rural areas have a low temperature. The temperature begins to rise in suburban residential areas with trees, then climbs higher in commercial areas. The temperature is highest in cities. The temperature begins to decrease in urban residential areas, then dips lower in parks. The temperature rises again in suburban residential ares without trees, then decreased in rural farmland. Courtesy of littlerock.gov<\/figcaption>\n<\/figure>\n<\/div>\n\n\n\n

The study identified wind speed as the strongest and most consistent driver of urban heat island intensity, with higher winds reducing temperature differences between urban and rural areas throughout the year. Other weather factors, including temperature and precipitation, influenced the urban heat island differently depending on the season. <\/p>\n\n\n\n

The researchers also documented more frequent “inverted” heat islands \u2014 periods when urban areas were actually cooler than surrounding rural landscapes \u2014 than had previously been observed in Madison or comparable cities. Together, the findings underscore the importance of long-term, year-round monitoring to better understand local climate patterns and provide valuable insights for designing and evaluating strategies to reduce urban heat in Madison and cities around the world.<\/p>\n","protected":false},"excerpt":{"rendered":"

An extensive sensor network reveals how Madison’s urban heat island changes from season to season \u2014 and why it matters for climate planning.<\/p>\n","protected":false},"author":5,"featured_media":52643,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":"","_links_to":"","_links_to_target":""},"categories":[1],"tags":[],"post_template":[],"class_list":["post-52583","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-uncategorized"],"acf":[],"yoast_head":"\nTaking the City's Temperature | The Commons Magazine<\/title>\n<meta name=\"description\" content=\"On some days, Madison's streets and buildings trap enough heat to make the city noticeably warmer than the surrounding countryside.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" 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