Abstract:Abstract. Most precipitation from deep clouds over the continents and in the intertropical convergence zone is strongly influenced by the presence of ice crystals whose formation requires the presence of ice nucleating particles (INPs). Although there are a large number of INP sources, the ice nucleating abilities of aerosol particles originating from oceans, deserts, and wildfires are poorly described at tropical latitudes. To fill this gap in knowledge, the National Autonomous University of Mexico micro-orif… Show more
“…Tegen and Fung (1995) and Tegen et al (2004) also proposed that the PSD of the aerosol particles can vary according to soil type. The size of the aerosol particles is well known to influence their behavior as INPs (Diehl and Wurzler, 2004;DeMott et al, 2010;Mason et al, 2015b;Córdoba et al, 2021). This fact is evidenced in the different PSD distributions observed for each sample in Fig.…”
Section: Ice Nucleating Abilitiesmentioning
confidence: 86%
“…The ice nucleating abilities of the agricultural dust particles collected in the field and generated in the laboratory were analyzed through the immersion freezing mode using the UNAM-MOUDI-DFT (Córdoba et al, 2021). The equipment consisted of (a) a cold stage, (b) a humid/dry air system, (c) a Zeiss Axio Scope A1 optical microscope (Axiolab Zeiss) with a recording system, and (d) a data acquisition system (Córdoba et al, 2021).…”
Abstract. Agricultural soil erosion, both mechanical and eolic, may impact
cloud processes, as some aerosol particles are able to facilitate ice crystal formation. Given the large agricultural sector in Mexico, this study investigates the ice nucleating abilities of agricultural dust collected at different sites and generated in the laboratory. The immersion freezing mechanism of ice nucleation was simulated in the laboratory via the Universidad Nacional Autónoma de México (UNAM) microorifice
uniform deposit impactor (MOUDI) droplet freezing technique (DFT), i.e.,
UNAM-MOUDI-DFT. The results show that agricultural dust from the Mexican
territory promote ice formation in the temperature range from
−11.8 to −34.5 ∘C, with ice nucleating particle (INP) concentrations between 0.11 and 41.8 L−1. Furthermore, aerosol samples generated in the laboratory are more efficient than those collected in the field, with T50 values (i.e., the temperature at which 50 % of the droplets freeze) higher by more than 2.9 ∘C. Mineralogical analysis indicated a high concentration of feldspars, i.e., K-feldspar and plagioclase (>40 %), in most of the aerosol and soil samples, with K-feldspar significantly correlated with the T50 of particles with aerodynamic diameters between 1.8 and 3.2 µm. Similarly, the organic carbon (OC) was correlated with the ice nucleation efficiency of aerosol samples from 3.2 to 5.6 and from 1.0 to 1.8 µm. Finally, a decrease in INP efficiency after heating the samples at 300 ∘C for 2 h indicates that the organic matter from agricultural soils plays a predominant role in the ice nucleating abilities of this type of aerosol sample.
“…Tegen and Fung (1995) and Tegen et al (2004) also proposed that the PSD of the aerosol particles can vary according to soil type. The size of the aerosol particles is well known to influence their behavior as INPs (Diehl and Wurzler, 2004;DeMott et al, 2010;Mason et al, 2015b;Córdoba et al, 2021). This fact is evidenced in the different PSD distributions observed for each sample in Fig.…”
Section: Ice Nucleating Abilitiesmentioning
confidence: 86%
“…The ice nucleating abilities of the agricultural dust particles collected in the field and generated in the laboratory were analyzed through the immersion freezing mode using the UNAM-MOUDI-DFT (Córdoba et al, 2021). The equipment consisted of (a) a cold stage, (b) a humid/dry air system, (c) a Zeiss Axio Scope A1 optical microscope (Axiolab Zeiss) with a recording system, and (d) a data acquisition system (Córdoba et al, 2021).…”
Abstract. Agricultural soil erosion, both mechanical and eolic, may impact
cloud processes, as some aerosol particles are able to facilitate ice crystal formation. Given the large agricultural sector in Mexico, this study investigates the ice nucleating abilities of agricultural dust collected at different sites and generated in the laboratory. The immersion freezing mechanism of ice nucleation was simulated in the laboratory via the Universidad Nacional Autónoma de México (UNAM) microorifice
uniform deposit impactor (MOUDI) droplet freezing technique (DFT), i.e.,
UNAM-MOUDI-DFT. The results show that agricultural dust from the Mexican
territory promote ice formation in the temperature range from
−11.8 to −34.5 ∘C, with ice nucleating particle (INP) concentrations between 0.11 and 41.8 L−1. Furthermore, aerosol samples generated in the laboratory are more efficient than those collected in the field, with T50 values (i.e., the temperature at which 50 % of the droplets freeze) higher by more than 2.9 ∘C. Mineralogical analysis indicated a high concentration of feldspars, i.e., K-feldspar and plagioclase (>40 %), in most of the aerosol and soil samples, with K-feldspar significantly correlated with the T50 of particles with aerodynamic diameters between 1.8 and 3.2 µm. Similarly, the organic carbon (OC) was correlated with the ice nucleation efficiency of aerosol samples from 3.2 to 5.6 and from 1.0 to 1.8 µm. Finally, a decrease in INP efficiency after heating the samples at 300 ∘C for 2 h indicates that the organic matter from agricultural soils plays a predominant role in the ice nucleating abilities of this type of aerosol sample.
“…Subsequently, the glass coverslips were placed in stages 5 and 6 (cut sizes of 1.0 and 0.56 µm, respectively) of an 8-stage Micro Orifice Uniform Deposit Impactor (MOUDI, Model 100R, MSP Corp.) 36 . The glass plates were fixed onto the MOUDI stages by substrate holders, as reported by Córdoba et al (2021) 37 . The MOUDI inlet flow was calibrated before sampling to 30 L/min using a Gilibrator air flow calibrator (Sensidyne, Inc., Clearwater, Florida, USA).…”
More than 7 thousand wildfires were recorded over Mexico in 2019, affecting almost 640 thousand hectares. Most of these fires occurred during the spring season generating dense smoke plumes, impacting urban areas in the central part of the Mexican plateau. From May 10 to 17, 2019, biomass burning (BB) plumes affected Mexico City (MC) and diffused across the basin, producing PM2.5 levels ~ 2 times higher than the nation's air quality standards. Average PM2.5 concentrations increased sharply from 29.4 ± 7.2 µg m−3 to 65.1 ± 13.6 µg m−3 when the dense smoke plumes were detected. The higher particle concentration impacted the aerosol optical depth (AOD) as values ~ 3 times greater than the annual mean (0.32 ± 0.12) were measured, which resulted in a 17% loss of global horizontal irradiation (GHI). Under these severe pollution conditions, the visibility (Va) was reduced by ~ 80%. The high incidence of strong absorbent particles, such as soot and tarballs was revealed through electron microscopy and X-ray fluorescence (XRF) analysis. These techniques show chemical similarities between MC aerosols and those from the high-altitude (~ 4010 m. a. g. l.) Altzomoni Atmospheric Observatory, evidencing a strong influence of the BB emissions, suggesting a regional transport of these pollutants.
“…Subsequently, the glass coverslips were placed in stages 5 and 6 (cut sizes of 1.0 and 0.56 µm, respectively) of an 8-stage Micro Ori ce Uniform Deposit Impactor (MOUDI, Model 100R, MSP Corp.) 56 . The glass plates were xed onto the MOUDI stages by substrate holders, as reported by Córdoba et al (2021) 57 . The MOUDI inlet ow was calibrated before sampling to 30 L/min using a Gilibrator air ow calibrator (Sensidyne, Inc., Clearwater, Florida, USA).…”
More than 7 thousand wildfires were recorded over Mexico in 2019, affecting almost 640 thousand hectares. Most of these fires occurred during the warm-dry season generating dense smoke plumes, impacting urban areas in the central part of the Mexican plateau. From May 10 to 17, 2019, biomass burning (BB) plumes affected Mexico City (MC) and diffused across the basin, drastically reducing visibility. Due to the severity of this high atmospheric pollution (HAP) episode, the local government declared an environmental contingency, warning the population. Fine particle (PM2.5) concentrations were ~ 2 times higher than the nation's air quality standards. Likewise, aerosol optical measurements indicated that visibility was mainly affected by fine aerosol particles. Electron microscopy analysis of aerosol samples obtained during the HAP days shows a high incidence of strong absorbent soot and tarballs (TB). These types of particles were simultaneously observed in MC and at the high-altitude Altzomoni Atmospheric Observatory (~ 4010 m.a.g.l.). Elemental analysis of the particles shows that the composition is dominated by sulfur and potassium, evidencing a strong influence of the BB emissions, but also suggests the presence of urban pollution from MC at the remote Altzomoni site.
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