Some aspects of boundary layer evolution in Mexico City |
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Authors: | G. B. Raga D. Baumgardner G. Kok I. Rosas |
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Affiliation: | a Centro de Ciencias de la Atmósfera, UNAM, Ciudad Universitaria, 04510 México City, Mexico;b National Center for Atmospheric Research, Boulder, CO, USA |
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Abstract: | Measurements of chemical species and meteorological parameters were made at a site located 440 m above the mean basin level of Mexico City, over a two-week period in November during Project Azteca. Data from three of the stations of Mexico City's air quality monitoring network (Red Automática de Monitoreo Ambiental, RAMA) were also used to estimate the dilution in concentration experienced by pollutants as they are transported upslope during the course of the day. Both carbon monoxide and sulfur dioxide show a dilution of up to 50%, while ozone is usually more concentrated at the elevated site. These comparisons clearly highlight the intrinsic differences between primary and secondary gases, which are supported also by time–space, cross correlation analysis. The thermal mesoscale wind circulation dominates concentrations of pollutants at the research site: upslope during the day and downslope during the night. The data present clear evidence that downslope flows during the night contribute to ozone concentration at basin sites. |
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Keywords: | Air quality Pollution transport in complex topography Megacity pollutants |
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