Marine stratocumulus clouds often become decoupled from the vertical layer immediately above the ocean surface. This study contrasts cloud chemical composition between coupled and decoupled marine stratocumulus clouds for dissolved nonwater substances. Cloud water and droplet residual particle composition were measured in clouds off the California coast during three airborne experiments in July-August of separate years (Eastern Pacific Emitted Aerosol Cloud Experiment 2011, Nucleation in California Experiment 2013, and Biological and Oceanic Atmospheric Study 2015). Decoupled clouds exhibited significantly lower air-equivalent mass concentrations in both cloud water and droplet residual particles, consistent with reduced cloud droplet number concentration and subcloud aerosol (D-p>100nm) number concentration, owing to detachment from surface sources. Nonrefractory submicrometer aerosol measurements show that coupled clouds exhibit higher sulfate mass fractions in droplet residual particles, owing to more abundant precursor emissions from the ocean and ships. Consequently, decoupled clouds exhibited higher mass fractions of organics, nitrate, and ammonium in droplet residual particles, owing to effects of long-range transport from more distant sources. Sodium and chloride dominated in terms of air-equivalent concentration in cloud water for coupled clouds, and their mass fractions and concentrations exceeded those in decoupled clouds. Conversely, with the exception of sea-salt constituents (e.g., Cl, Na, Mg, and K), cloud water mass fractions of all species examined were higher in decoupled clouds relative to coupled clouds. Satellite and Navy Aerosol Analysis and Prediction System-based reanalysis data are compared with each other, and the airborne data to conclude that limitations in resolving boundary layer processes in a global model prevent it from accurately quantifying observed differences between coupled and decoupled cloud composition.

Airborne aerosols are crucial atmospheric constituents that are involved in global climate change and human life qualities. Understanding the nature and magnitude of aerosol-cloud-precipitation interactions is critical in model predictions for atmospheric radiation budget and the water cycle. The interactions depend on a variety of factors including aerosol physicochemical complexity, cloud types, meteorological and thermodynamic regimes and data processing techniques. This PhD work is an effort to quantify the relationships among aerosol, clouds, and precipitation on both global and regional scales by using satellite retrievals and aircraft measurements. The first study examines spatial distributions of conversion rate of cloud water to rainwater in warm maritime clouds over the globe by using NASA A-Train satellite data. This study compares the time scale of the onset of precipitation with different aerosol categories defined by values of aerosol optical depth, fine mode fraction, and Ångstrom Exponent. The results indicate that conversion time scales are actually quite sensitive to lower tropospheric static stability (LTSS) and cloud liquid water path (LWP), in addition to aerosol type. Analysis shows that tropical Pacific Ocean is dominated by the highest average conversion rate while subtropical warm cloud regions (far northeastern Pacific Ocean, far southeastern Pacific Ocean, Western Africa coastal area) exhibit the opposite result. Conversion times are mostly shorter for lower LTSS regimes. When LTSS condition is fixed, higher conversion rates coincide with higher LWP and lower aerosol index categories. After a general global view of physical property quantifications, the rest of the presented PhD studies is focused on regional airborne observations, especially bulk cloud water chemistry and aerosol aqueous-phase reactions during the summertime off the California coast. Local air mass origins are categorized into three distinct types (ocean, ships, and land) with their influences on cloud water composition examined and implications of wet deposition discussed. Chemical analysis of cloud water samples indicates a wide pH range between 2.92 and 7.58, with an average as 4.46. The highest pH values were observed north of San Francisco, coincident with the strongest land mass influence (e.g. Si, B, and Cs). Conversely, the lowest pH values were observed south of San Francisco where there is heavy ship traffic, resulting in the highest concentrations of sulfate, nitrate, V, Fe, Al, P, Cd, Ti, Sb, P, and Mn. The acidic cloud environment with influences from various air mass types can affect the California coastal aquatic ecosystem since it can promote the conversion of micronutrients to more soluble forms. Beyond characterization of how regional air mass sources affect cloud water composition, aircraft cloud water collection provides precious information on tracking cloud processing with specific species such as oxalic acid, which is the most abundant dicarboxylic acid in tropospheric aerosols. Particular attention is given to explore relationship between detected metals with oxalate aqueous-phase production mechanisms. A number of case flights show that oxalate concentrations drop by nearly an order of magnitude relative to samples in the same vicinity with similar environmental and cloud physical conditions. Such a unique feature was consistent with an inverse relationship between oxalate and Fe. In order to examine the hypothesis that oxalate decreasing is potentially related to existing of Fe, chemistry box model simulations were conducted. The prediction results show that the loss of oxalate due to the photolysis of iron oxalato complexes is likely a significant oxalate sink in the study region due to the ubiquity of oxalate precursors, clouds, and metal emissions from ships, the ocean, and continental sources.

Le milieu nuageux est un milieu complexe au sein duquel un grand nombre d’espèces chimiques peuvent être transformées. Dans ce cadre, la caractérisation chimique et la réactivité photochimique de la phase aqueuse des nuages ont été étudiées. La caractérisation chimique de la phase aqueuse des nuages a permis de montrer que les masses d’air échantillonnées au sommet du puy de Dôme sont majoritairement sous trois influences distinctes, à savoir océanique, continentale et anthropique. La distribution des paramètres physicochimiques et des composés inorganiques est dépendante du type de masses d’air échantillonnées. De plus, la quantification des acides carboxyliques et des aldéhydes a permis de mettre en avant la complexité de la matière organique avec la présence d’une multitude de composés encore non identifiés. L’étude de la réactivité photochimique de la phase aqueuse des nuages a également été réalisée, montrant que la capacité photooxydante de la phase aqueuse des nuages ainsi que les vitesses de dégradation de différentes espèces chimiques sont plus importantes pour les masses d’air polluées. Pour la première fois, des vitesses de photoproduction des radicaux hydroxyles ont été évaluées dans la phase aqueuse des nuages, montrant que les ions nitrates et le peroxyde d’hydrogène sont des sources photochimiques majeures des radicaux hydroxyles (représentant jusqu’à 80 % de leur photoproduction totale). / Clouds represent complex media where many species can be transformed. In order to characterize the chemical composition of cloud water and to better understand the processes involved in the transformations of these species, the characterization and the photoreactivity of cloud water were studied. The characterization of cloud water showed that air masses sampled at the puy de Dôme station can be subject to different influences (marine, continental and anthropogenic). The distribution of the physicochemical parameters and of inorganic compounds was different for each kind of air masses. Moreover, the quantification of carboxylic acids and aldehydes showed the complexity of the organic matter contained in cloud water, with the presence of many unknown organic compounds. The photoreactivity of cloud water was also studied, showing that the oxidizing capacity of cloud water and the degradation rate of organic compounds were higher in polluted air masses. For the first time, hydroxyl radical formation rates were determined in cloud water sampled at the puy de Dôme station, showing that nitrate ions and hydrogen peroxide are among the main sources of hydroxyl radicals (contributing up to 80 % of their total photoformation).

科学研究費補助金 研究種目:一般研究(C) 課題番号:63540311 研究代表者:石坂 隆 研究期間:1988-1989年度