Titlebook: Regional Climate Variability and its Impacts in the Mediterranean Area; A. Mellouki,A. R. Ravishankara Conference proceedings 2007 Springe

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Aerosols in Global Models – Focus on Europe They exert an opposite to greenhouse gases effect on the global atmospheric temperature by decelerating the warming of the climate. Global 3-dimensional models have to account for the atmospheric processes that affect aerosols in the atmosphere, namely emissions, nucleation, condensation, evaporati

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Non-Methane Volatile Organic Compound Measurements in the City Centre of Wroclaw, Polands in the city of Wroclaw, Poland. The measurements covered NMVOCs in the range of C.-C.. Samples were collected using Carbotrap and Carbosieve SIII solid adsorption tubes and analysed off-line by thermal desorption and GC-FID analysis. Measurements were performed on purpose to assess the contributio

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Pcos971

Representation of Chemical Detail in Atmospheric Modelsunds (VOCs). The basis of the protocols used for constructing the MCM is described, together with the website used for dissemination. A number of applications is briefly discussed, including policy development, support for field measurements and the formation of secondary organic aerosol. Heterogene

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Photoenhanced Uptake of NO2 on Mineral Dustke of different gases, such as NO. (mainly as HNO. or N.O.), on the solid surfaces exhibited by the uplifted minerals. While such “dark” processes have been deeply studied over the last years, dust particles contain a series of oxides that may be initiate photochemical process that have not been con

Torrid

Gas Phase Processes Relevant to the Mediterranean Some New and Important Topicsther the intention has been to try and highlight work that has been going on gas-phase processes which have possible important conesquences for the complex chemistry occurring in the Mediterranean atmosphere. The manuscript is constrained to chemical processes involved in the gas-phase photooxidatio

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Representation of Chemical Detail in Atmospheric Modelsications is briefly discussed, including policy development, support for field measurements and the formation of secondary organic aerosol. Heterogeneous uptake has been incorporated into the MCM and the difficulties involved are summarized. Finally, an aqueous phase mechanism, CAPRAM is outlined.