The Progressive Increase of the Urban Heat Island’s Influence on Temperature Records
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Perhaps no other climatic variable receives more attention in the debate over CO2-induced global warming than temperature. Its forecast change over time in response to rising atmospheric CO2 concentrations is the typical measure by which climate models are compared. It is also the standard by which the climate model projections tend to be judged; right or wrong, the correctness of global warming theory is most often adjudicated by comparing model projections of temperature against real-world measurements. And in such comparisons, it is critical to have a proper baseline of good data; but that is easier acknowledged than accomplished, as multiple problems and potential inaccuracies have been identified in even the best of temperature datasets.
One particular issue in this regard is the urban heat island effect, a phenomenon by which urban structures artificially warm background air temperatures above what they normally would be in a non-urbanized environment. The urban influence on a given station’s temperature record can be quite profound. In large cities, for example, urban-induced heating can be as great as Tokyo’s 10°C, making it all the more difficult to detect and discern a CO2-induced global warming signal in the temperature record, especially since the putative warming of non-urbanized areas of the planet over the past century is believed to be less than 1°C. Yet, because nearly all long-term temperature records have been obtained from sensors initially located in towns and cities that have experienced significant growth over the past century, it is extremely important that urbanization-induced warming -- which can be a full order of magnitude greater than the background trend being sought -- be removed from the original temperature records when attempting to accurately assess the true warming (or cooling!) of the natural non-urban environment. A new study by Founda et al. (2015) suggests this may not be so simple or straightforward a task.
Working with temperature records in and around the metropolitan area of Athens, Greece, Founda et al. set out to examine the interdecadal variability of the urban heat island (UHI) effect, since “few studies focus on the temporal variability of UHI intensity over long periods.” Yet, as they note, “knowledge of the temporal variability and trends of UHI intensity is very important in climate change studies, since [the] urban effect has an additive effect on long term air temperature trends.”
To complete their objective the four Greek researchers compared long-term air temperature data from two urban, two suburban and two rural stations over the period 1970-2004. The UHI was calculated as the difference between the urban and suburban (or rural) stations for monthly, seasonal and annual means of air temperature (max, min, and mean).
Among their several findings, the authors report notable differences in the UHI’s intensity across the seasons and in comparing the UHI when calculated using maximum, minimum, or mean temperatures. Of significance to the discussion at hand, however, the authors note “the warming rate of the air temperature in Athens is particularly large during [the] last decades,” such that the “difference of the annual mean air temperature between urban and rural stations exhibited a progressively statistically significant increase over the studied period.” Indeed, as shown in the figure below for the stations (a) National Observatory of Athens (NOA) in the center of Athens and Tanagra (TAN), approximately 50 km north of the city, as well as for (b) the coastal urban station of Hellinikon (HEL) and again the rural station of Tanagra, the anthropogenic influence of urbanization on temperatures at these two urban stations is growing in magnitude with time such that “the mean values of UHI magnitude [calculated across the entire record] are not quite representative of the more recent period.”
Interdecadal variation and annual trends of the Athens, Greece UHI calculated between two urban and one rural station using mean annual temperatures over the period 1970-2004. The two urban stations were the National Observatory of Athens (NOA) in the center of Athens and Hellinikon (HEL), located near the urbanized coast. The rural station Tanagra (TAN), was located approximately 50 km north of the city. Adapted from Founda et al. (2015).
Such findings as these are of significant relevance in climate change studies, for they clearly indicate the UHI influence on a temperature record is not static. It changes over time and is likely inducing an ever-increasing warming bias on the temperature record, a bias that will only increase as the world’s population continues to urbanize in the years and decades ahead. Consequently, unless researchers routinely identify and remove this growing UHI influence from the various temperature data bases used in global change studies, there will likely be a progressive overestimation of the influence of the radiative effects of rising CO2 on the temperature record.
Reference
Founda, D., et al. 2015. Interdecadal variations and trends of the Urban Heat Island in Athens (Greece) and its response to heat waves. Atmospheric Research, 161-162, 1-13.
