4.5 Article

Effects of fireworks on particulate matter concentration in a narrow valley: the case of the Medellin metropolitan area

Journal

ENVIRONMENTAL MONITORING AND ASSESSMENT
Volume 192, Issue 1, Pages -

Publisher

SPRINGER
DOI: 10.1007/s10661-019-7838-9

Keywords

Atmospheric boundary layer; Air quality; Atmospheric stability; Black carbon; Fireworks; Particulate matter

Funding

  1. SIATA (Sistema de Alerta Temprana de Medellin y el Valle de Aburra) funds by Area Metropolitana del Valle de Aburra (AMVA), Municipio de Medellin
  2. Grupo EPM
  3. ISAGEN [CD511]
  4. Universidad EAFIT
  5. Universidad Nacional de Colombia under the Facultad de Minas graduate scholarship program

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The extensive use of fireworks generates large amounts of pollutants, deteriorating air quality and potentially causing adverse health impacts. In Medellin and its metropolitan area, although fireworks are banned during December, their use is widespread during the Christmas season, particularly during the midnight of November 30 (La Alborada) and New Year's Eve (NYE). It is therefore essential to assess the effects of these celebrations on air quality in the region. Air-quality data from the official monitoring network and a low-cost particulate matter (PM) citizen science project, backscattering intensity (BI) retrievals from a ceilometer network, potential temperature from a microwave radiometer, and information from a radar wind profiler provide an excellent platform to study the spatio-temporal distribution of contaminants resulting from the La Alborada and NYE celebrations. Substantial increases in PM2.5 and PM10 mass concentrations due to La Alborada and NYE, ranging in some cases from 50 to 100 mu gm(-3), are observed in the Aburra Valley and particularly in the densely populated communes of Medellin, with most concentration changes corresponding to ultrafine and fine particles. The PM increments resulting from fireworks show almost no increase in the net amount of black carbon in the atmosphere. Ceilometer BI profiles show a substantial change immediately after the La Alborada and NYE midnights, confined to the atmospheric boundary layer (ABL). Strong thermal inversions lead to fairly homogeneous increments in BI within the ABL, lasting until the onset of the convective boundary layer. In contrast, weak thermal inversions lead to rapid dispersion of aerosols, allowing them to episodically escape above the ABL.

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