Abstract

Abstract. The concentration of gases and aerosol particles have been measured at the mountain site of Altzomoni, 4010 m in altitude, located 60 km southeast of Mexico City, 50 km east of Puebla and 70 km northeast of Cuernavaca. The objective of this study was to evaluate the properties of gases and particles in the Regional Mixed Layer (RML) of Mexico's Megapolis. Altzomoni is generally above the RML from late evening until late morning at which time the arrival of the RML is marked by increasing concentrations of CO and aerosol particles that reach their maxima in mid-afternoon. The average diurnal cycles for fourteen days in March, 2006 were evaluated during which time the synoptic scale circulation had three principal patterns: from the east (E), southwest (SW) and west northwest (WNW). The original hypothesis was that air arriving from the direction of Mexico City would have much higher concentrations of anthropogenic gases and particles than air from Puebla or Cuernavaca, due to the relatively large differences in populations. In fact, not only were the average, maximum concentrations of CO and O3 (0.3 and 0.1 ppmv) approximately the same for air originating from the WNW and E, but the average maximum concentrations of Peroxyacyl nitrates (PAN,PPN) and particle organic matter (POM) in air from the E exceeded those in air from the WNW. Comparisons of measurements from the mountain site with those made by aircraft during the same period, using the same type of aerosol mass spectrometer, show that the total masses of POM, NO3−, SO42− and NH4+ were approximately the same from aircraft measurements made over Mexico City and when winds were from the east at the mountain site. In contrast 75% of the total aerosol mass at the mountain site was POM whereas over Mexico City the fraction of POM was less than 60%. The measurements suggest the occasional influence of emissions from the nearby volcano, Popocatepetl, as well as possible incursions of biomass combustion; however, the large concentrations of O3, PAN and POM suggest that secondary processes are the major source for these gases and particles. The similar concentrations in gases and particles when air is coming from the E and NWN raises the possibility of recirculation of air from Mexico City and the importance of this mechanism for impacting the regional air quality.

Highlights

  • In the central plateau region of Mexico, 33% of the country’s population resides in Mexico City and in the states of Morelos, Mexico, Puebla, Tlaxcala and Queretaro, i.e. approximately 36 million inhabitants living in a region the size of Switzerland but five times the population

  • In addition to its strategic location with respect to nearby urban areas, there are no significant local sources of anthropogenic contaminants since it is situated in the national park of Izta-Popo-Zoquiapan with only a single road nearby that is principally used to bring weekend tourists to the park center and is approximately five km to the southeast of the research site

  • Measurements of gas and particle properties, made on the Altzomoni ridge located at an altitude of 4010 m in the Pass of Cortez between the volcanoes of Popocatepetl and Iztaccıhuatl in the central region of the Mexican Megapolis, have been evaluated with respect to the direction of flow and the diurnal fluctuations of the Regional Mixed Layer (RML)

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Summary

Introduction

In the central plateau region of Mexico, 33% of the country’s population resides in Mexico City and in the states of Morelos, Mexico, Puebla, Tlaxcala and Queretaro, i.e. approximately 36 million inhabitants living in a region the size of Switzerland but five times the population. This region has been designated a Megapolis by local authorities (Proaire, 2007) where a Megapolis is defined as an extensive metropolitan area or a group of continuous metropolitan areas (Gottmann, 1957). D. Baumgardner et al.: Pollution in the regional mixed layer of central Mexico operations, motor vehicle traffic and cooking (Proaire, 2007). A large fraction of this area is agricultural or forested and during some months of the year biomass burning, intentional or inadvertent, makes a significant contribution to the poor air quality in the Megapolis (Molina et al, 2007; Bravo et al, 2002; Salcedo et al, 2006) when it intensifies in late March, reaching a maximum in May each year (Fast et al, 2007; Bravo et al, 2002)

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