Analysis of secondary organic aerosol simulation bias in the Community Earth System Model (CESM2.1)
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Published:2021-05-26
Issue:10
Volume:21
Page:8003-8021
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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:
Liu Yaman, Dong XinyiORCID, Wang MinghuaiORCID, Emmons Louisa K.ORCID, Liu Yawen, Liang YuanORCID, Li Xiao, Shrivastava ManishORCID
Abstract
Abstract. Organic aerosol (OA) has been considered as one of the
most important uncertainties in climate modeling due to the complexity in
presenting its chemical production and depletion mechanisms. To better
understand the capability of climate models and probe into the associated
uncertainties in simulating OA, we evaluate the Community Earth System Model
version 2.1 (CESM2.1) configured with the Community Atmosphere Model version
6 (CAM6) with comprehensive tropospheric and stratospheric chemistry
representation (CAM6-Chem) through a long-term simulation (1988–2019) with
observations collected from multiple datasets in the United States. We find
that CESM generally reproduces the interannual variation and seasonal cycle
of OA mass concentration at surface layer with a correlation of 0.40 compared to ground observations and systematically overestimates (69 %)
in summer and underestimates (−19 %) in winter. Through a series of
sensitivity simulations, we reveal that modeling bias is primarily related
to the dominant fraction of monoterpene-formed secondary organic aerosol
(SOA), and a strong positive correlation of 0.67 is found between
monoterpene emission and modeling bias in the eastern US during summer. In terms
of vertical profile, the model prominently underestimates OA and monoterpene
concentrations by 37 %–99 % and 82 %–99 %, respectively, in the upper air
(> 500 m) as validated against aircraft observations. Our study
suggests that the current volatility basis set (VBS) scheme applied in CESM
might be parameterized with monoterpene SOA yields that are too high, which
subsequently results in strong SOA production near the emission source area. We
also find that the model has difficulty in reproducing the decreasing trend
of surface OA in the southeastern US probably because of employing pure gas VBS to
represent isoprene SOA which is in reality mainly formed through multiphase
chemistry; thus, the influence of aerosol acidity and sulfate particle change
on isoprene SOA formation has not been fully considered in the model. This
study reveals the urgent need to improve the SOA modeling in climate models.
Funder
National Natural Science Foundation of China Ministry of Science and Technology of the People's Republic of China
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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