An intensive two-week study of an urban CO₂ dome in Phoenix, Arizona, USA

Atmospheric CO₂ concentrations were measured prior to dawn and in the middle of the afternoon at a height of 2m above the ground along four transects through the metropolitan area of Phoenix, Arizona on 14 consecutive days in January 2000. The data revealed the existence of a strong but variable urban CO₂ dome, which at one time exhibited a peak CO₂ concentration at the center of the city that was 75% greater than that of the surrounding rural area. Mean city-center peak enhancements, however, were considerably lower, averaging 43% on weekdays and 38% on weekends; and averaged over the entire commercial sector of the city, they were lower still, registering 30% on weekdays and 23% on weekends. Over the surrounding residential areas, on the other hand, there are no weekday-weekend differences in boundary-layer CO₂ concentration. Furthermore, because of enhanced vertical mixing during the day, near-surface CO₂ concentrations in the afternoon are typically reduced from what they are prior to sunrise. This situation is additionally perturbed by the prevailing southwest-to-northeast flow of air at that time of day, which lowers afternoon CO₂ concentrations on the southern and western edges of the city still more, as a consequence of the importation of pristine rural air. The southwest-to-northeast flow of air also sometimes totally compensates for the afternoon vertical-mixing-induced loss of CO₂ from areas on the northern and eastern sides of the city, as a consequence of the northeastward advection of CO₂ emanating from the central, southern and western sectors of the city. Hence, although complex, the nature of the urban CO₂ dome of Phoenix, Arizona, is readily understandable in terms of basic meteorological phenomena and their interaction with human activities occurring at the land/air interface. Copyright (C) 2001 .