Eoghan Darbyshire
University of Manchester
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Publication
Featured researches published by Eoghan Darbyshire.
Nucleation and Atmospheric Aerosols | 2013
W. T. Morgan; J. D. Allan; M. Flynn; Eoghan Darbyshire; Amy K. Hodgson; Ben Johnson; James M. Haywood; Saulo R. Freitas; Karla M. Longo; Paulo Artaxo; Hugh Coe
Biomass burning represents one of the largest sources of particulate matter to the atmosphere, which results in a significant perturbation to the Earth’s radiative balance coupled with serious negative impacts on public health. Globally, biomass burning aerosols are thought to exert a small warming effect of 0.03 Wm−2, however the uncertainty is 4 times greater than the central estimate. On regional scales, the impact is substantially greater, particularly in areas such as the Amazon Basin where large, intense and frequent burning occurs on an annual basis for several months (usually from August-October). Furthermore, a growing number of people live within the Amazon region, which means that they are subject to the deleterious effects on their health from exposure to substantial volumes of polluted air. Initial results from the South American Biomass Burning Analysis (SAMBBA) field experiment, which took place during September and October 2012 over Brazil, are presented here. A suite of instrumentation wa...
Atmospheric Chemistry and Physics | 2018
C. L. Reddington; W. T. Morgan; Eoghan Darbyshire; Joel Brito; Hugh Coe; Paulo Artaxo; John H. Marsham; D. V. Spracklen
Biomass burning is a major source of particulate matter pollution, regionally and globally. This has important implications for air quality and climate. Over South America, intense fires occur in August-September typically, providing the dominating source of atmospheric aerosols to the region. Yet considerable uncertainties in the magnitude of fire emissions remain. As such, the paper focuses on ‘improving understanding of aerosol emissions from vegetation fires’ by considering three different fire emission datasets (namely GFED4.1, GFAS1.2 and FINN1.5) to account for fire emissions in their modelling work. The authors used a global aerosol model (GLOMAP) to study how the simulated particulate matter (PM) concentration and aerosol optical thickness (AOT) are affected by the three different fire emission inventories. These results are compared against a comprehensive set of surface, aircraft and satellite observations collected over the Amazon region during September 2012. The authors have highlighted the spatial and temporal variation in the three different fire emissions and how it affects simulated quantities. Overall, the authors conclude that GLOMAP has skill in predicting reasonable surface concentration and vertical profile of PM over South America despite noticeable differences between the emission inventories. However, GLOMAP simulated AOT is found to be systematically underestimated. The authors therefore recommend caution when evaluating global models using AOTs to constrain particulate emissions from fires.
NUCLEATION AND ATMOSPHERIC AEROSOLS: 19th International Conference | 2013
Amy K. Hodgson; W. T. Morgan; Eoghan Darbyshire; J. D. Allan; Hugh Coe
Biomass burning is a huge source of atmospheric aerosols and is poorly understood leading to large uncertainties in estimates of radiative forcing of climate. Aerosols have both a direct effect on climate by reflecting and absorbing solar radiation and an indirect effect by acting as cloud condensation nuclei (CCN) and ice nuclei (IN). Biomass burning aerosols are produced from burning of vegetation with the vast majority occurring in the tropics. This research presents data collected during the aircraft campaign of the South American Biomass Burning Analysis (SAMBBA) project during September and October 2012. A smouldering rainforest fire and a flaming savannah-like fire were selected for in-depth case studies of the atmospheric plume constituents and provide a comparison between the two fire types. The physiochemical characterization of the two plumes are identified, with preliminary results showing a significant difference in the black carbon concentration of the two plumes; 6μg m−3 for the smouldering...
Atmospheric Chemistry and Physics | 2015
Claire L. Ryder; J. B. McQuaid; Cyrille Flamant; Phil Rosenberg; Richard Washington; Helen E. Brindley; Ellie Highwood; John H. Marsham; Douglas J. Parker; Martin C. Todd; James Banks; Jennifer Brooke; Sebastian Engelstaedter; V. Estellés; P. Formenti; Luis Garcia-Carreras; Cécile Kocha; Franco Marenco; Harald Sodemann; Christopher S. Allen; Aurelien Bourdon; M. Bart; Carolina Cavazos-Guerra; Servanne Chevaillier; Jonathan Crosier; Eoghan Darbyshire; Angela R. Dean; J. R. Dorsey; Joss Kent; Debbie O'Sullivan
Atmospheric Chemistry and Physics | 2014
J. D. Allan; P. I. Williams; J. Najera; J. D. Whitehead; M. Flynn; J. W. Taylor; Dantong Liu; Eoghan Darbyshire; Lucy J. Carpenter; Rosemary Jane Chance; Stephen J. Andrews; S. C. Hackenberg; Gordon McFiggans
Atmospheric Chemistry and Physics | 2015
Dantong Liu; Boris Quennehen; Eoghan Darbyshire; J. D. Allan; P. I. Williams; J. W. Taylor; S. J.-B. Bauguitte; M. Flynn; Douglas Lowe; Martin Gallagher; Keith N. Bower; T. W. Choularton; Hugh Coe
Atmospheric Chemistry and Physics | 2014
J. D. Allan; W. T. Morgan; Eoghan Darbyshire; M. Flynn; P. I. Williams; D. E. Oram; Paulo Artaxo; Joel Brito; James Lee; Hugh Coe
Geoscientific Model Development | 2014
Scott Archer-Nicholls; Douglas Lowe; Eoghan Darbyshire; W. T. Morgan; Megan M. Bela; Gabriel Pereira; J. Trembath; Johannes W. Kaiser; Karla M. Longo; Saulo R. Freitas; Hugh Coe; Gordon McFiggans
Atmospheric Chemistry and Physics | 2016
J. D. Whitehead; Eoghan Darbyshire; Joel Brito; Henrique M. J. Barbosa; Ian Crawford; Rafael Stern; Martin Gallagher; Paul H. Kaye; J. D. Allan; Hugh Coe; Paulo Artaxo; Gordon McFiggans
Atmospheric Chemistry and Physics | 2016
Ben Johnson; James M. Haywood; Justin M. Langridge; Eoghan Darbyshire; W. T. Morgan; Kate Szpek; Jennifer Brooke; Franco Marenco; Hugh Coe; Paulo Artaxo; Karla M. Longo; J. Mulcahy; G. W. Mann; Mohit Dalvi; Nicolas Bellouin