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Precipitating cloud‐system response to aerosol perturbations
Author(s) -
Lee SeoungSoo,
Feingold Graham
Publication year - 2010
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2010gl045596
Subject(s) - aerosol , atmospheric sciences , precipitation , convection , troposphere , environmental science , scavenging , perturbation (astronomy) , forcing (mathematics) , seeding , supersaturation , climatology , meteorology , chemistry , geology , physics , thermodynamics , biochemistry , quantum mechanics , antioxidant
We simulate aerosol effects on a Tropical Western Pacific mixed‐phase convective cloud system of two‐day duration that is well constrained by observations. This facilitates exploration of aerosol‐induced changes in precipitation pathways. A 10‐fold increase in aerosol produces a small (9%) increase in the simulated precipitation due to an enhancement in convective rain countering a reduction in stratiform rain. A more distinct feature is that in stratiform clouds, precipitation efficiency PE and scavenging efficiency SE decrease significantly with increasing aerosol. There is very close agreement between PE and SE both temporally and for stratiform vs. convective rain. The time required for the perturbed system to relax back to the unperturbed aerosol state is ∼10 days, with only weak sensitivity to the magnitude of the aerosol perturbation and the modeled increase (or decrease) in precipitation. The upper tropospheric relaxation time is substantially longer, with implications for direct forcing and heterogeneous chemistry.