Aerosol responses to precipitation along North American air trajectories arriving at Bermuda
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Published:2021-11-02
Issue:21
Volume:21
Page:16121-16141
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Dadashazar Hossein, Alipanah MajidORCID, Hilario Miguel Ricardo A.ORCID, Crosbie Ewan, Kirschler Simon, Liu HongyuORCID, Moore Richard H.ORCID, Peters Andrew J., Scarino Amy Jo, Shook MichaelORCID, Thornhill K. Lee, Voigt ChristianeORCID, Wang HailongORCID, Winstead Edward, Zhang BoORCID, Ziemba Luke, Sorooshian Armin
Abstract
Abstract. North American pollution outflow is ubiquitous over the western North
Atlantic Ocean, especially in winter, making this location a suitable
natural laboratory for investigating the impact of precipitation on aerosol
particles along air mass trajectories. We take advantage of observational
data collected at Bermuda to seasonally assess the sensitivity of aerosol
mass concentrations and volume size distributions to accumulated
precipitation along trajectories (APT). The mass concentration of
particulate matter with aerodynamic diameter less than 2.5 µm
normalized by the enhancement of carbon monoxide above background
(PM2.5/ΔCO) at Bermuda was used to estimate the degree of
aerosol loss during transport to Bermuda. Results for December–February
(DJF) show that most trajectories come from North America and have the highest
APTs, resulting in a significant reduction (by 53 %) in PM2.5/ΔCO under high-APT conditions (> 13.5 mm) relative to low-APT
conditions (< 0.9 mm). Moreover, PM2.5/ΔCO was most
sensitive to increases in APT up to 5 mm (−0.044 µg m−3 ppbv−1 mm−1) and less sensitive to increases in APT over 5 mm.
While anthropogenic PM2.5 constituents (e.g., black carbon, sulfate,
organic carbon) decrease with high APT, sea salt, in contrast, was comparable
between high- and low-APT conditions owing to enhanced local wind and sea
salt emissions in high-APT conditions. The greater sensitivity of the fine-mode volume concentrations (versus coarse mode) to wet scavenging is evident
from AErosol RObotic NETwork
(AERONET) volume size distribution data. A combination of GEOS-Chem model
simulations of the 210Pb submicron aerosol tracer and its gaseous precursor
222Rn reveals that (i) surface aerosol particles at Bermuda are most
impacted by wet scavenging in winter and spring (due to large-scale
precipitation) with a maximum in March, whereas convective scavenging plays
a substantial role in summer; and (ii) North American 222Rn tracer
emissions contribute most to surface 210Pb concentrations at Bermuda in
winter (∼ 75 %–80 %), indicating that air masses arriving at
Bermuda experience large-scale precipitation scavenging while traveling from
North America. A case study flight from the ACTIVATE field campaign on 22 February 2020 reveals a significant reduction in aerosol number and volume
concentrations during air mass transport off the US East Coast associated
with increased cloud fraction and precipitation. These results highlight the
sensitivity of remote marine boundary layer aerosol characteristics to
precipitation along trajectories, especially when the air mass source is
continental outflow from polluted regions like the US East Coast.
Funder
National Aeronautics and Space Administration National Science Foundation
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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