Direct and Indirect Effects of Precipitation on Particulate Matter Concentration in the Aburrá Valley
Abstract
Wet deposition, including in-cloud scavenging (ICS) and below-cloud scavenging (BCS), is one of the most important processes of particulate matter (PM) removal from the atmosphere. ICS mainly refers to the growth of particulates into cloud droplets, whereas BCS consists of collisions and coalescence between raindrops and pollutants. The overall influence of precipitation in the concentration of fine particulate matter less than 2.5 microns in size (PM2.5) in the Medellín metropolitan area located in the narrow Aburrá Valley within the Colombian Andes is assessed using weather radar derived precipitation with 5 minutes resolution and hourly data from air quality monitoring stations from the Medellín Early Warning System ( Sistema de Alerta Temprana de Medellin y el Valle de Aburra -SIATA-) monitoring network. A non-parametric probabilistic analysis is proposed in order to understand the net influence of precipitation within the diurnal cycle. Probability density functions (PDF) of PM2.5 concentration during precipitations events as well as under dry conditions are analyzed for every hour of the day. The overlapping coefficient for these distributions was used, along with the Wilcoxon Mann-Whitney test, in order to summarized the net effect of precipitation in aerosol concentration. Evidence suggests that, while there is a clear and significant role of precipitation in aerosol concentration, the net effect is contrasting and strongly depends on the diurnal cycle of atmospheric stability. During stable conditions in the lower troposphere, typically occurring during the night and before midmorning, evidence suggest that precipitation reduces the near-surface PM2.5 concentration due to an effective BCS resulting in net negative forcing. On the other hand, when a precipitation event takes place during the day, when the lower troposphere is typically unstable, the PM2.5 concentration increases, suggesting an net positive forcing given that the BCS is offset by the atmospheric stabilization effect of precipitation, which in turns results in near-surface PM accumulation.
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2017
- Bibcode:
- 2017AGUFM.A44D..07R
- Keywords:
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- 0345 Pollution: urban and regional;
- ATMOSPHERIC COMPOSITION AND STRUCTURE;
- 0365 Troposphere: composition and chemistry;
- ATMOSPHERIC COMPOSITION AND STRUCTURE;
- 0368 Troposphere: constituent transport and chemistry;
- ATMOSPHERIC COMPOSITION AND STRUCTURE