2009Journal of Geophysical Research AtmospheresRequires access

Marine stratocumulus aerosol‐cloud relationships in the MASE‐II experiment: Precipitation susceptibility in eastern Pacific marine stratocumulus

Miao‐Ling Lu, Armin Sorooshian, Haflidi H. Jonsson, Graham Feingold, Richard C. Flagan, John H. Seinfeld

Open publisher page 88 citations

Abstract

Observational data on aerosol‐cloud‐drizzle relationships in marine stratocumulus are presented from the second Marine Stratus/Stratocumulus Experiment (MASE‐II) carried out in July 2007 over the eastern Pacific near Monterey, California. Observations, carried out in regions of essentially uniform meteorology with localized aerosol enhancements due to ship exhaust (“ship tracks”), demonstrate, in accord with those from numerous other field campaigns, that increased cloud drop number concentration Nc and decreased cloud top effective radius re are associated with increased subcloud aerosol concentration. Modulation of drizzle by variations in aerosol levels is clearly evident. Variations of cloud base drizzle rate Rcb are found to be consistent with the proportionality, Rcb ∝ H3/Nc, where H is cloud depth. Simultaneous aircraft and A‐Train satellite observations are used to quantify the precipitation susceptibility of clouds to aerosol perturbations in the eastern Pacific region.

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What this paper is about

Observational data on aerosol‐cloud‐drizzle relationships in marine stratocumulus are presented from the second Marine Stratus/Stratocumulus Experiment (MASE‐II) carried out in July 2007 over the eastern Pacific near Monterey, California. Observations, carried out in regions of essentially uniform meteorology with localized aerosol enhancements due to ship exhaust (“ship tracks”), demonstrate, in accord with those from numerous other field campaigns, that increased cloud drop number concentration Nc and decreased cloud top effective radius re are associated with increased subcloud aerosol concentration. Modulation of drizzle by variations in aerosol levels is clearly evident. Variations of cloud base drizzle rate Rcb are found to be consistent with the proportionality, Rcb ∝ H3/Nc, where H is cloud depth. Simultaneous aircraft and A‐Train satellite observations are used to quantify the precipitation susceptibility of clouds to aerosol perturbations in the eastern Pacific region.

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Available abstract

Observational data on aerosol‐cloud‐drizzle relationships in marine stratocumulus are presented from the second Marine Stratus/Stratocumulus Experiment (MASE‐II) carried out in July 2007 over the eastern Pacific near Monterey, California. Observations, carried out in regions of essentially uniform meteorology with localized aerosol enhancements due to ship exhaust (“ship tracks”), demonstrate, in accord with those from numerous other field campaigns, that increased cloud drop number concentration Nc and decreased cloud top effective radius re are associated with increased subcloud aerosol concentration. Modulation of drizzle by variations in aerosol levels is clearly evident. Variations of cloud base drizzle rate Rcb are found to be consistent with the proportionality, Rcb ∝ H3/Nc, where H is cloud depth. Simultaneous aircraft and A‐Train satellite observations are used to quantify the precipitation susceptibility of clouds to aerosol perturbations in the eastern Pacific region.

Key concepts: Drizzle, Marine stratocumulus, Aerosol, Environmental science, Atmospheric sciences, Cloud top, Effective radius, Meteorology

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