Vertical structure of biomass burning aerosol transported over the southeast Atlantic Ocean
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Published:2022-08-03
Issue:15
Volume:22
Page:9859-9876
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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:
Harshvardhan HarshvardhanORCID, Ferrare Richard, Burton Sharon, Hair Johnathan, Hostetler Chris, Harper David, Cook Anthony, Fenn Marta, Scarino Amy Jo, Chemyakin Eduard, Müller DetlefORCID
Abstract
Abstract. Biomass burning in southwestern Africa produces smoke plumes that
are transported over the Atlantic Ocean and overlie vast regions of
stratocumulus clouds. This aerosol layer contributes to direct and indirect
radiative forcing of the atmosphere in this region particularly during the
months of August, September, and October. There was a multi-year
international campaign to study this aerosol and its interactions with
clouds. Here, we report on the evolution of aerosol distributions and
properties as measured by the airborne high spectral resolution lidar
(HSRL-2) during the ORACLES (Observations of Aerosols above Clouds and their
intEractionS) campaign in September 2016. The NASA Langley HSRL-2 instrument
was flown on the NASA ER-2 aircraft for several days in September 2016. Data
were aggregated at two pairs of 2∘ × 2∘ grid
boxes to examine the evolution of the vertical profile of aerosol properties
during transport over the ocean. Results showed that the structure of the
profile of aerosol extinction and microphysical properties is maintained
over a 1 to 2 d timescale. In the 3–5 km altitude range, 95 % of
the aerosol extinction was contributed by particles in the 0.05–0.50 µm radius size range with the aerosol in this size range having an average
effective radius of 0.16 µm. This indicates that there is essentially
no scavenging or dry deposition at these altitudes. Moreover, there is very
little day-to-day variation in these properties, such that time sampling as
happens in such campaigns may be representative of longer periods such as
monthly means. Below 3 km, there is considerable mixing with larger aerosol,
most likely continental source near land. Furthermore, these measurements
indicated that there was often a distinct gap between the bottom of the
aerosol layer and cloud tops at the selected locations as evidenced by a
layer of several hundred meters that contained relatively low aerosol
extinction values above the clouds.
Funder
Earth Sciences Division
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference63 articles.
1. Adebiyi, A. A., Zuidema, P., Chang, I., Burton, S. P., and Cairns, B.: Mid-level clouds are frequent above the southeast Atlantic stratocumulus clouds, Atmos. Chem. Phys., 20, 11025–11043, https://doi.org/10.5194/acp-20-11025-2020, 2020. 2. Anderson, T. L., Charlson, R. J., Winker, D. M., Ogren, J. A., and
Holmén, K.: Mesoscale variations of tropospheric aerosols, J. Atmos.
Sci., 60, 119–136, 2003. 3. Anderson, T. L., Wu, Y., Chu, D. A., Schmid, B., Redemann, J., and Dubovik,
O.: Testing the MODIS satellite retrieval of aerosol fine-mode fraction, J.
Geophys. Res., 110, D18204, https://doi.org/10.1029/2005JD005978, 2005. 4. Boucher, O., Randall, D., Artaxo, P., Bretherton, C., Feingold, G., Forster,
P., Kerminen, V.-M. Kondo, Y., Liao, H., Lohmann, U., Rasch, P., Satheesh,
S. K., Sherwood, S., Stevens B., and Zhang, X. Y.: Clouds and Aerosols, in:
Climate Change 2013: The Physical Science Basis. Contribution of Working
Group I to the Fifth Assessment Report of the Intergovernmental Panel on
Climate Change, edited by: Stocker, T. F., Qin, D., Plattner, G.-K., Tignor, M., Allen,
S. K., Boschung, J., Nauels, A., Xia, Y., Bex V., and Midgley, P. M., Cambridge University Press, 571–657,
https://doi.org/10.1017/CBO9781107415324.016, 2013. 5. Buchard, V., Randles, C. A., da Silva, A. M., Darmenov, A., Colarco, P. R.,
Govindaraju, R., Ferrare, R. A., Hair, J., Beyersdorf, A. J. Ziemba L. D.,
and Yu, H.: The MERRA-2 aerosol reanalysis, 1980 onwards Part II: Evaluation
and case studies, J. Climate, 30, 6851–6871, https://doi.org/10.1175/JCLI-D-16-0613.1,
2017.
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