Annual exposure to polycyclic aromatic hydrocarbons in urban environments linked to wintertime wood-burning episodes Atmospheric Chemistry and Physics DOI 10.5194/acp-21-17865-2021 25 February 2022 We analyse observations from year-long measurements at Athens, Greece. Nighttime wintertime PAH levels are 4 times higher than daytime, and wintertime values are 15 times higher than summertime. Biomass burning aerosol during wintertime pollution events is responsible for these significant wintertime enhancements and accounts for 43 % of the population exposure to PAH carcinogenic risk. Biomass burning poses additional health risks beyond those associated with the high PM levels that develop. Read more
A sulfur dioxide Covariance-Based Retrieval Algorithm (COBRA): application to TROPOMI reveals new emission sources Atmospheric Chemistry and Physics DOI 10.5194/acp-21-16727-2021 28 January 2022 We present a new algorithm to retrieve sulfur dioxide from space UV measurements. We apply the technique to high-resolution TROPOMI measurements and demonstrate the high sensitivity of the approach to weak SO2 emissions worldwide with an unprecedented limit of detection of 8 kt yr-1. This result has broad implications for atmospheric science studies dealing with improving emission inventories and identifying and quantifying missing sources, in the context of air quality and climate. COBRA): application to TROPOMI reveals new emission sources">Read more
An Arctic ozone hole in 2020 if not for the Montreal Protocol Atmospheric Chemistry and Physics DOI 10.5194/acp-21-15771-2021 10 January 2022 We use satellite and balloon measurements to evaluate modeled ozone loss seen in the unusually cold Arctic of 2020 in the real world and compare it to simulations of a world avoided. We show that extensive denitrification in 2020 provides an important test case for stratospheric model process representations. If the Montreal Protocol had not banned ozone-depleting substances, an Arctic ozone hole would have emerged for the first time in spring 2020 that is comparable to those in the Antarctic. Read more
Self-consistent global transport of metallic ions with WACCM-X Atmospheric Chemistry and Physics DOI 10.5194/acp-21-15619-2021 3 January 2022 Metal layers occur in the MLT region (80–120 km) from the ablation of cosmic dust. The latest lidar observations show these metals can reach a height approaching 200 km, which is challenging to explain. We have developed the first global simulation incorporating the full life cycle of metal atoms and ions. The model results compare well with lidar and satellite observations of the seasonal and diurnal variation of the metals and demonstrate the importance of ion mass and ion-neutral coupling. WACCM-X">Read more
Direct estimates of biomass burning NOx emissions and lifetimes using daily observations from TROPOMI Atmospheric Chemistry and Physics DOI 10.5194/acp-21-15569-2021 31 December 2021 We describe direct estimates of NOx emissions and lifetimes for biomass burning plumes using daily TROPOMI retrievals of NO2. Satellite-derived NOx emission factors are consistent with those from in situ measurements. We observe decreasing NOx lifetime with fire intensity, which is due to the increase in NOx abundance and radical production. Our findings suggest promise for applying space-based observations to track the emissions and chemical evolution of reactive nitrogen from wildfires. TROPOMI">Read more
How alkaline compounds control atmospheric aerosol particle acidity Atmospheric Chemistry and Physics DOI 10.5194/acp-21-14983-2021 22 December 2021 Aerosol particle pH is well-buffered by alkaline compounds, notably NH3 and crustal elements. NH3 is found to supply remarkable buffering capacity on a global scale, from the polluted continents to the remote oceans. Potential future changes in agricultural NH3 must be accompanied by strong reductions of SO2 and NOx to avoid particles becoming highly acidic, with implications for human health (aerosol toxicity), ecosystems (acid deposition), clouds, and climate (aerosol hygroscopicity). Read more
Aerosol–cloud interactions: the representation of heterogeneous ice activation in cloud models Atmospheric Chemistry and Physics DOI 10.5194/acp-21-15213-2021 20 December 2021 Aerosol–cloud interactions play an important role in climate change. Simulations of the competition between homogeneous solution droplet freezing and heterogeneous ice nucleation can be compromised by the misapplication of ice-active particle fractions frequently derived from laboratory measurements or parametrizations. Our study frames the problem and establishes a solution that is easy to implement in cloud models. Read more
Ambient aerosol properties in the remote atmosphere from global-scale in situ measurements Atmospheric Chemistry and Physics DOI 10.5194/acp-21-15023-2021 15 December 2021 The Atmospheric Tomography Mission was an airborne study that mapped the chemical composition of the remote atmosphere. From this, we developed a comprehensive description of aerosol properties that provides a unique, global-scale dataset against which models can be compared. The data show the polluted nature of the remote atmosphere in the Northern Hemisphere and quantify the contributions of sea salt, dust, soot, biomass burning particles, and pollution particles to the haziness of the sky. Read more
The driving factors of new particle formation and growth in the polluted boundary layer Atmospheric Chemistry and Physics DOI 10.5194/acp-21-14275-2021 19 November 2021 Experiments at CLOUD show that in polluted environments new particle formation (NPF) is largely driven by the formation of sulfuric acid–base clusters, stabilized by amines, high ammonia concentrations or lower temperatures. While oxidation products of aromatics can nucleate, they play a minor role in urban NPF. Our experiments span 4 orders of magnitude variation of observed NPF rates in ambient conditions. We provide a framework based on NPF and growth rates to interpret ambient observations. Read more
Heterogeneity and chemical reactivity of the remote troposphere defined by aircraft measurements Atmospheric Chemistry and Physics DOI 10.5194/acp-21-13729-2021 3 November 2021 The NASA Atmospheric Tomography (ATom) mission built a climatology of the chemical composition of tropospheric air parcels throughout the middle of the Pacific and Atlantic oceans. The level of detail allows us to reconstruct the photochemical budgets of O3 and CH4 over these vast, remote regions. We find that most of the chemical heterogeneity is captured at the resolution used in current global chemistry models and that the majority of reactivity occurs in the “hottest” 20 % of parcels. Read more