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Titel |
Evaluation of factors controlling global secondary organic aerosol production from cloud processes |
VerfasserIn |
C. He, J. Liu, A. G. Carlton, S. Fan, L. W. Horowitz, H. Levy II, S. Tao |
Medientyp |
Artikel
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Sprache |
Englisch
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ISSN |
1680-7316
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Digitales Dokument |
URL |
Erschienen |
In: Atmospheric Chemistry and Physics ; 13, no. 4 ; Nr. 13, no. 4 (2013-02-19), S.1913-1926 |
Datensatznummer |
250017667
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Publikation (Nr.) |
copernicus.org/acp-13-1913-2013.pdf |
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Zusammenfassung |
Secondary organic aerosols (SOA) exert a significant influence on ambient
air quality and regional climate. Recent field, laboratorial and modeling
studies have confirmed that in-cloud processes contribute to a large
fraction of SOA production with large space-time heterogeneity. This study
evaluates the key factors that govern the production of cloud-process SOA
(SOAcld) on a global scale based on the GFDL coupled chemistry-climate
model AM3 in which full cloud chemistry is employed. The association between
SOAcld production rate and six factors (i.e., liquid water content
(LWC), total carbon chemical loss rate (TCloss), temperature,
VOC/NOx, OH, and O3) is examined. We find that LWC alone
determines the spatial pattern of SOAcld production, particularly over
the tropical, subtropical and temperate forest regions, and is strongly
correlated with SOAcld production. TCloss ranks the second and
mainly represents the seasonal variability of vegetation growth. Other
individual factors are essentially uncorrelated spatiotemporally to
SOAcld production. We find that the rate of SOAcld production is
simultaneously determined by both LWC and TCloss, but responds linearly
to LWC and nonlinearly (or concavely) to TCloss. A parameterization
based on LWC and TCloss can capture well the spatial and temporal
variability of the process-based SOAcld formation (R2 = 0.5)
and can be easily applied to global three dimensional models to represent
the SOA production from cloud processes. |
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