Justin J. N. Lingard
University of Leeds
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Featured researches published by Justin J. N. Lingard.
Bulletin of the American Meteorological Society | 2009
Curtis R. Wood; Samantha J. Arnold; Ahmed A. Balogun; Janet F. Barlow; Stephen E. Belcher; Re Britter; Hong Cheng; Adrian Dobre; Justin J. N. Lingard; Damien Martin; Marina K.-A. Neophytou; Fredrik K. Petersson; Alan Robins; Dudley E Shallcross; R.J. Smalley; James Tate; Alison S. Tomlin; Iain R. White
In the event of a release of toxic gas in the center of London, emergency services personnel would need to determine quickly the extent of the area contaminated. The transport of pollutants by turbulent flow within the complex streets and building architecture of London, United Kingdom, is not straightforward, and we might wonder whether it is at all possible to make a scientifically reasoned decision. Here, we describe recent progress from a major U.K. project, Dispersion of Air Pollution and its Penetration into the Local Environment (DAPPLE; information online at www.dapple.org.uk). In DAPPLE, we focus on the movement of airborne pollutants in cities by developing a greater understanding of atmospheric flow and dispersion within urban street networks. In particular, we carried out full-scale dispersion experiments in central London from 2003 through 2008 to address the extent of the dispersion of tracers following their release at street level. These measurements complemented previous studies because 1...
Bulletin of the American Meteorological Society | 2009
Ian M. Brooks; Margaret J. Yelland; Robert C. Upstill-Goddard; Philip D. Nightingale; S. D. Archer; Ericic d'Asaro; Rachael Beale; Cory M. Beatty; B. W. Blomquist; A. Anthony Bloom; Barbara J. Brooks; John Cluderay; David Coles; John W. H. Dacey; Michael D. DeGrandpre; Jo Dixon; William M. Drennan; Joseph Gabriele; Laura Goldson; Nick J. Hardman-Mountford; Martin K. Hill; Matt Horn; Ping-Chang Hsueh; Barry J. Huebert; Gerrit de Leeuw; T.G. Leighton; M.I. Liddicoat; Justin J. N. Lingard; Craig McNeil; J. B. McQuaid
As part of the U.K. contribution to the international Surface Ocean–Lower Atmosphere Study, a series of three related projects—DOGEE, SEASAW, and HiWASE—undertook experimental studies of the processes controlling the physical exchange of gases and sea spray aerosol at the sea surface. The studies share a common goal: to reduce the high degree of uncertainty in current parameterization schemes. The wide variety of measurements made during the studies, which incorporated tracer and surfactant release experiments, included direct eddy correlation fluxes, detailed wave spectra, wind history, photographic retrievals of whitecap fraction, aerosol-size spectra and composition, surfactant concentration, and bubble populations in the ocean mixed layer. Measurements were made during three cruises in the northeast Atlantic on the RRS Discovery during 2006 and 2007; a fourth campaign has been making continuous measurements on the Norwegian weather ship Polarfront since September 2006. This paper provides an overview of the three projects and some of the highlights of the measurement campaigns.
Journal of Environmental Monitoring | 2006
Justin J. N. Lingard; David T. Young; Gordon E. Andrews; Alison S. Tomlin
A summertime study of the number concentration and the size distribution of combustion derived nanometre sized particles (termed nanoparticles) from diesel and spark-ignition (SI) engine emissions were made under rush-hour and free-flow traffic conditions at an urban roadside location in Leeds, UK in July 2003. The measured total particle number concentrations (N(TOTAL)) were of the order 1.8 x 10(4) to 3.4 x 10(4) cm(-3), and tended to follow the diurnal traffic flow patterns. The N(TOTAL) was dominated by particles < or =100 nm in diameter which accounted for between 89-93% of the measured particle number. By use of a log-normal fitting procedure, the modal parameters of the number based particle size distribution of urban airborne particulates were derived from the roadside measurements. Four component modes were identified. Two nucleation modes were found, with a smaller, more minor, mode composed principally of sub-11 nm particles, believed to be derived from particles formed from the nucleation of gaseous species in the atmosphere. A second mode, much larger in terms of number, was composed of particles within the size range of 10-20 nm. This second mode was believed to be principally derived from the condensation of the unburned fuel and lube oil (the solvent organic fraction or SOF) as it cooled on leaving the engine exhaust. Third and fourth modes were noted within the size ranges of 28-65 nm and 100-160 nm, respectively. The third mode was believed to be representative of internally mixed Aitken mode particles composed of a soot/ash core with an adsorbed layer of readily volatilisable material. The fourth mode was believed to be composed of chemically aged, secondary particles. The larger nucleation and Aitken modes accounted for between 80-90% of the measured N(TOTAL), and the particles in these modes were believed to be derived from SI and diesel engine emissions. The overall size distribution, particularly in modes II-IV, was observed to be strongly related to the number of primary particle emissions, with larger count median diameters observed under conditions where low numbers of primary soot based particles were present.
Journal of Environmental Monitoring | 2008
Justin J. N. Lingard; Alison S. Tomlin
Measurements of concentrations and size distributions of particles 4.7 to 160 nm were taken using an SMPS during the bonfire and firework celebrations on Bonfire Night in Leeds, UK, 2006. These celebrations provided an opportunity to study size distributions in a unique atmospheric pollution situation during and following a significant emission event due to open biomass burning. A log-normal fitting program was used to determine the characteristics of the modal groups present within hourly averaged size distributions. Results from the modal fitting showed that on bonfire night the smallest nucleation mode, which was present before and after the bonfire event and on comparison weekends, was not detected within the size distribution. In addition, there was a significant shift in the modal diameters of the remaining modes during the peak of the pollution event. Using the concept of a coagulation sink, the atmospheric lifetimes of smaller particles were significantly reduced during the pollution event, and thus were used to explain the disappearance of the smallest nucleation mode as well as changes in particle count mean diameters. The significance for particle mixing state is discussed.
Bulletin of the American Meteorological Society | 2009
Ian M. Brooks; Margaret J. Yelland; Robert C. Upstill-Goddard; Philip D. Nightingale; Stephen D. Archer; Eric A. D'Asaro; Rachael Beale; Cory M. Beatty; B. W. Blomquist; A. Anthony Bloom; Barbara J. Brooks; John Cluderay; David Coles; John W. H. Dacey; Michael D. DeGrandpre; Jo Dixon; William M. Drennan; Joseph Gabriele; Laura Goldson; Nick J. Hardman-Mountford; Martin K. Hill; Matt Horn; Ping-Chang Hsueh; Barry J. Huebert; Gerrit de Leeuw; T.G. Leighton; M.I. Liddicoat; Justin J. N. Lingard; Craig McNeil; J. B. McQuaid
This document is a supplement to “Physical Exchanges at the Air–Sea Interface: UK–SOLAS Field Measurements,” by Ian M. Brooks, Margaret J. Yelland, Robert C. Upstill-Goddard, Philip D. Nightingale, Steve Archer, Eric d’Asaro, Rachael Beale, Cory Beatty, Byron Blomquist, A. Anthony Bloom, Barbara J. Brooks, John Cluderay, David Coles, John Dacey, Michael DeGrandpre, Jo Dixon, William M. Drennan, Joseph Gabriele, Laura Goldson, Nick Hardman-Mountford, Martin K. Hill, Matt Horn, Ping-Chang Hsueh, Barry Huebert, Gerrit de Leeuw, Timothy G. Leighton, Malcolm Liddicoat, Justin J. N. Lingard, Craig McNeil, James B. McQuaid, Ben I. Moat, Gerald Moore, Craig Neill, Sarah J. Norris, Simon O’Doherty, Robin W. Pascal, John Prytherch, Mike Rebozo, Erik Sahlee, Matt Salter, Ute Schuster, Ingunn Skjelvan, Hans Slagter, Michael H. Smith, Paul D. Smith, Meric Srokosz, John A. Stephens, Peter K. Taylor, Maciej Telszewski, Roisin Walsh, Brian Ward, David K. Woolf, Dickon Young, and Henk Zemmelink (Bull. Amer. Meteor. Soc., 90, 629–644) • ©2009 American Meteorological Society • Corresponding author: Ian M. Brooks, Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds LS2 9JT, United Kingdom • E-mail: [email protected] • DOI:10.1175/2008BAMS2578.2
Journal of Physics: Conference Series | 2009
Alison S. Tomlin; David T. Young; Justin J. N. Lingard; E L Agius
High time resolution, size segregated studies of ultrafine particle number concentrations (PNC) were performed at two UK roadside locations using a DMS500 particle spectrometer including sampling with and without a thermodenuder. Intercomparisons between the DMS500, an SMPS and a CPC, indicate that the SMPS can underestimate PNC due to the transient nature of excursions in concentrations and the longer scan time of the instrument. Short duration transient periods of high number concentrations made considerable contributions to hourly average PNC. The transient nature of changes in PNC potentially affects the type of exposure experienced in the roadside environment, as well as indoor outdoor exchange. The transient shifts were dominated by Aitken mode particles during high traffic periods, with the Aitken mode comprised of internally mixed particles with a low volatility core (thought to be primarily soot) and a surface of condensed and absorbed material. Transient periods of high nucleation mode PNC were also found, but were relatively more important during night-time and afternoon periods, due to secondary formation processes and lower concentrations of pre-existing particles. The thermodenuder studies indicated the presence of highly volatile liquid droplets in the nucleation mode which were lost on heating. Transient events and complexities in particle mixing state within the ultrafine fraction, coupled with discrepancies between instruments, make the potential adoption of a total number based air quality standard more complicated than first appears. Nucleation mode particle numbers are highly dependant on atmospheric and traffic conditions as well as pre-existing particle surface area and may be toxicologically less significant if they are predominantly liquid droplets. Aitken mode particles have been shown in previous studies to have higher toxicological significance due to their chemical composition. Their hourly average PNC correlated well with PM2.5 and estimated PM1 with lower significance of equivalent correlation of nucleation mode particles.
Archive | 2007
Justin J. N. Lingard; Barbara J. Brooks; Sarah J. Norris; Ian M. Brooks; Michael H. Smith
C.D. O’Dowd and P.E. Wagner (eds.), Nucleation and Atmospheric Aerosols, 1050–1054.
Atmospheric Environment | 2005
Justin J. N. Lingard; Alison S. Tomlin; A.G. Clarke; Katherine Healey; Alastair Hay; Christopher P. Wild; Michael N. Routledge
Atmospheric Chemistry and Physics | 2007
Sarah J. Norris; Ian M. Brooks; G. de Leeuw; Michael H. Smith; M.M. Moerman; Justin J. N. Lingard
Science of The Total Environment | 2007
David T. Young; Justin J. N. Lingard; R.J. Smalley; James Tate; Paul Goodman; Alison S. Tomlin