The Urban Heat Island of Mexicali, Mexico
Garcia Cueto, O.R., Martinez, A.T., Morales, G.B. 2009. Urbanization effects upon the air temperature in Mexicali, B.C., Mexico. Atmosfera 22: 349-365.
Working with daily records of maximum and minimum temperature from six weather stations "in Mexicali City and its surroundings" covering the period 1950-2000, and with "a climatic network of rural and urban weather stations in Mexicali and its valley and the Imperial Valley, California" over the "contemporary period (2000-2005)," Garcia Cueto et al. characterized the spatial and temporal development of the city's urban heat island over the latter half of the 20th century and the first five years of the 21st century. What they found was that Mexicali City "changed from being a cold island (1960-1980) to a heat island with a maximum intensity of 2.3°C in the year 2000, when it was compared with rural weather stations of Imperial, California," noting that "the replacement of irrigated agricultural land by urban landscapes, anthropogenic activity and population growth, appear to be the major factors responsible for the observed changes." And from the "more updated information (2000-2005)," they learned that "the greatest intensity of the urban heat island was in winter with a value of 5.7°C, and the lowest intensity in autumn with 5.0°C."
The results of this study clearly demonstrate that population growth and the clustering of people in cities can lead to localized warming (in areas where temperatures are routinely measured) that is both more rapid and much greater (by as much as an order of magnitude, in fact) than what the IPCC typically attempts to characterize as the "unprecedented" warming of the 20th century. And that population-growth-induced warming -- spread across the world -- has likely contributed, in large part, to what they wrongly construe to be CO2-induced global warming.