Quantifying the loss of processed natural gas within California’s South Coast Air Basin using long-term measurements of ethane and methane Atmospheric Chemistry and Physics DOI 10.5194/acp-16-14091-2016 15 November 2016 This paper investigates the cause of the known underestimate of bottom-up inventories of methane in California’s South Coast Air Basin (SoCAB). We use total column measurements of methane, ethane, carbon monoxide, and other trace gases beginning in the late 1980s to calculate emissions and attribute sources of excess methane to the atmosphere. We conclude that more than half of the excess methane to the SoCAB atmosphere is attributable to processed natural gas. Read more
The BErkeley Atmospheric CO2 Observation Network: initial evaluation Atmospheric Chemistry and Physics DOI 10.5194/acp-16-13449-2016 31 October 2016 We describe the design of and first results from the BErkeley Atmospheric CO2 Observation Network, a distributed instrument of 28 CO2 sensors stationed across and around the city of Oakland, California at ~ 2 km intervals. We evaluate the network via 4 performance parameters (cost, reliability, precision, systematic uncertainty) and find this high density technique to be sufficiently cost-effective and rigorous to inform understanding of small-scale urban emissions relevant to climate regulation. Read more
Optical properties and aging of light-absorbing secondary organic aerosol Atmospheric Chemistry and Physics DOI 10.5194/acp-16-12815-2016 14 October 2016 Light absorbing organic aerosols (BrC) absorb sunlight thereby influencing climate; however, understanding of the link between their optical properties and environmental variables remains limited. Our chamber experiment results suggest that variables including NOxconcentration, RH level, and photolysis time have considerable influence on secondary BrC optical properties. The results contribute to a more accurate characterization of the impacts of aerosols on climate, especially in urban areas. Read more
Screening of cloud microorganisms isolated at the Puy de Dôme (France) station for the production of biosurfactants Atmospheric Chemistry and Physics DOI 10.5194/acp-16-12347-2016 29 September 2016 A total of 480 microorganisms collected from 39 clouds sampled in France were isolated and identified. This unique collection was screened for biosurfactant production by measuring the surface tension. 41 % of the tested strains were active producers.Pseudomonas, the most frequently detected genus in clouds, was the dominant group for the production of biosurfactants. Further, the potential impact of the production of biosurfactants by cloud microorganisms on atmospheric processes is discussed. Read more
Long-term visibility variation in Athens (1931–2013): a proxy for local and regional atmospheric aerosol loads Atmospheric Chemistry and Physics DOI 10.5194/acp-16-11219-2016 12 September 2016 Historical time series are unique sources of information for past climate and atmospheric composition change. The 82-year time series of visibility data collected at the National Observatory of Athens (NOA) was an excellent proxy for the long-term evolution of particulate pollution in the eastern Mediterranean, at times when direct aerosol measurements were missing. Evolution of particulate pollution of both local and regional origin is nicely reflected on visibility records of NOA. Read more
Impacts of aviation fuel sulfur content on climate and human health Atmospheric Chemistry and Physics DOI 10.5194/acp-16-10521-2016 24 August 2016 Using a coupled tropospheric chemistry-aerosol microphysics model this research paper investigates the effect of variations in aviation fuel sulfur content (FSC) on surface PM2.5 concentrations, increases in aviation-induced premature mortalities, low-level cloud condensation nuclei and radiative effect. When investigating the climatic impact of variations in FSC the ozone direct radiative effect, aerosol direct radiative effect and aerosol cloud albedo effect are quantified. Read more
Satellite observations of stratospheric hydrogen fluoride and comparisons with SLIMCAT calculations Atmospheric Chemistry and Physics DOI 10.5194/acp-16-10501-2016 22 August 2016 HF, the dominant stratospheric fluorine reservoir, results from the atmospheric degradation of anthropogenic species such as CFCs, HCFCs, and HFCs. All are strong greenhouse gases, and CFCs and HCFCs deplete stratospheric ozone. We report the comparison of HF global distributions and trends measured by the ACE-FTS and HALOE satellite instruments with the output of SLIMCAT, a chemical transport model. The global HF trends reveal a slowing down in the rate of increase of HF since the 1990s. SLIMCAT calculations">Read more
Large gain in air quality compared to an alternative anthropogenic emissions scenario Atmospheric Chemistry and Physics DOI 10.5194/acp-16-9771-2016 4 August 2016 Three 30-year simulations of past atmospheric composition changes were performed using different anthropogenic emissions of pollutants accounting or not for the applied air quality legislation and accounting for the year–to–year observed climate and natural emissions variability. The actual benefit of applied legislation along with technological advances is higher than what is usually calculated by a simple comparison of today’s atmosphere against a constant anthropogenic emissions simulation. Read more
Growth of nucleation mode particles in the summertime Arctic: a case study Atmospheric Chemistry and Physics DOI 10.5194/acp-16-7663-2016 23 June 2016 We present a case study focused on an aerosol growth event observed in the Canadian High Arctic during summer. Using measurements of aerosol chemical and physical properties we find evidence for aerosol growth into cloud condensation nuclei-active sizes, through marine-influenced secondary organic aerosol formation. Understanding the mechanisms that control the formation and growth of aerosol is crucial for our ability to predict cloud properties, and therefore radiative balance and climate. Read more
Will a perfect model agree with perfect observations? The impact of spatial sampling Atmospheric Chemistry and Physics DOI 10.5194/acp-16-6335-2016 24 May 2016 We show that evaluating global aerosol model data with observations of very different spatial scales (200 vs. 10 km) can lead to large discrepancies, solely due to different spatial sampling. Strategies for reducing these sampling errors are developed and tested using a set of high-resolution model simulations. Read more