Premium
Representing effects of aqueous phase reactions in shallow cumuli in global models
Author(s) -
Nie Ji,
Kuang Zhiming,
Jacob Daniel J.,
Guo Jiahua
Publication year - 2016
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2015jd024208
Subject(s) - aqueous solution , plume , residence time (fluid dynamics) , flux (metallurgy) , reaction rate , thermal diffusivity , eddy diffusion , chemical reaction , environmental science , thermodynamics , atmospheric sciences , chemistry , materials science , meteorology , physics , turbulence , geology , biochemistry , geotechnical engineering , catalysis , organic chemistry
Aqueous phase reactions are important, sometimes dominant (e.g., for SO 2 ), pathways for the oxidation of air pollutants at the local and/or global scale. In many current chemical transport models (CTMs), the transport and aqueous reactions of chemical species are treated as split processes, and the subgrid‐scale heterogeneity between cloudy and environmental air is not considered. Here using large eddy simulation (LES) with idealized aqueous reactions mimicking the oxidation of surface‐originated SO 2 by H 2 O 2 in shallow cumuli, we show that the eddy diffusivity mass flux (EDMF) approach with a bulk plume can represent those processes quite well when entrainment/detrainment rates and eddy diffusivity are diagnosed using a conservative thermodynamic variable such as total water content. The reason is that a typical aqueous reaction such as SO 2 aqueous oxidation is relatively slow compared to the in‐cloud residence time of air parcels in shallow cumuli. As a result, the surface‐originated SO 2 is well correlated with and behaves like conservative thermodynamic variables that also have sources at the surface. Experiments with various reaction rate constants and relative abundances of SO 2 and H 2 O 2 indicate that when the reaction timescale approaches the in‐cloud residence time of air parcels, the errors of the bulk plume approach start to increase. Treating chemical tracer transport and aqueous reaction as split processes leads to significant errors, especially when the reaction is fast compared to the in‐cloud residence time. Overall, the EDMF approach shows large improvement over the CTM‐like treatments in matching the LES results.