0000000000131881

AUTHOR

J. N. Crowley

showing 6 related works from this author

Chemical and meteorological influences on the lifetime of NO<sub>3</sub> at a semirural mountain site during "PA…

2016

Abstract. Through measurements of NO2, O3, and NO3 during the PARADE campaign (PArticles and RAdicals, Diel observations of mEchanisms of oxidation) in the German Taunus mountains we derive nighttime, steady state lifetimes (τss) of NO3 and N2O5. During some nights, high NO3 (~ 200 pptv) and N2O5 (~ 1 ppbv) mixing ratios are associated with values of τss that exceeded one hour for NO3 and three hours for N2O5 near the ground. Such long boundary layer lifetimes for NO3 and N2O5 are usually only encountered in very clean/unreactive air masses whereas the PARADE measurement site is impacted by both biogenic emissions from the surrounding forest and anthropogenic emissions from the nearby urban…

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Diurnal variability, photochemical production and loss processes of hydrogen peroxide in the boundary layer over Europe

2019

Hydrogen peroxide (H2O2) plays a significant role in the oxidizing capacity of the atmosphere. It is an efficient oxidant in the liquid phase and serves as a temporary reservoir for the hydroxyl radical (OH), the most important oxidizing agent in the gas phase. Due to its high solubility, removal of H2O2 due to wet and dry deposition is efficient, being a sink of HOx (OH+HO2) radicals. In the continental boundary layer, the H2O2 budget is controlled by photochemistry, transport and deposition processes. Here we use in situ observations of H2O2 and account for chemical source and removal mechanisms to study the interplay between these processes. The data were obtained during five ground-base…

Atmospheric Science010504 meteorology & atmospheric sciencesUrbanisationEnvironment010502 geochemistry & geophysicsPhotochemistry01 natural scienceslcsh:QC1-999lcsh:ChemistryTroposphereBoundary layerchemistry.chemical_compoundDeposition (aerosol physics)lcsh:QD1-999chemistryOxidizing agentddc:550Environmental scienceSunriseHydroxyl radicalHydrogen peroxideEnvironment & SustainabilityDiel vertical migrationlcsh:Physics0105 earth and related environmental sciences
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Chemical and meteorological influences on the lifetime of NO3 at a semi-rural mountain site during PARADE

2016

Through measurements of NO2, O3 and NO3 during the PARADE campaign (PArticles and RAdicals, Diel observations of mEchanisms of oxidation) in the German Taunus mountains we derive nighttime steady-state lifetimes (τss) of NO3 and N2O5. During some nights, high NO3 (∼ 200 pptv) and N2O5 (∼ 1 ppbv) mixing ratios were associated with values of τss that exceeded 1 h for NO3 and 3 h for N2O5 near the ground. Such long boundary-layer lifetimes for NO3 and N2O5 are usually only encountered in very clean/unreactive air masses, whereas the PARADE measurement site is impacted by both biogenic emissions from the surrounding forest and anthropogenic emissions from the nearby urbanised/industrialised cen…

lcsh:Chemistrylcsh:QD1-999lcsh:Physicslcsh:QC1-999Atmospheric Chemistry and Physics
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Summertime total OH reactivity measurements from boreal forest during HUMPPA-COPEC 2010

2012

Ambient total OH reactivity was measured at the Finnish boreal forest station SMEAR II in Hyytiälä (Latitude 61°51' N; Longitude 24°17' E) in July and August 2010 using the Comparative Reactivity Method (CRM). The CRM – total OH reactivity method – is a direct, in-situ determination of the total loss rate of hydroxyl radicals (OH) caused by all reactive species in air. During the intensive field campaign HUMPPA-COPEC 2010 (<b>H</b>yytiälä <b>U</b>nited <b>M</b>easurements of <b>P</b>hotochemistry and <b>P</b>articles in <b>A</b>ir – <b>C</b>omprehensive <b>O</b>rganic <b>P&l…

0106 biological scienceslcsh:Chemistry010504 meteorology & atmospheric scienceslcsh:QD1-99913. Climate action15. Life on land01 natural scienceslcsh:Physicslcsh:QC1-999010606 plant biology & botany0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Influence of vessel characteristics and atmospheric processes on the gas and particle phase of ship emission plumes: in situ measurements in the Medi…

2020

A total of 252 emission plumes of ships operating in the Mediterranean Sea and around the Arabian Peninsula were investigated using a comprehensive dataset of gas- and submicron-particle-phase properties measured during the 2-month shipborne AQABA (Air Quality and Climate Change in the Arabian Basin) field campaign in summer 2017. The post-measurement identification of the corresponding ship emission events in the measured data included the determination of the plume sources (up to 38 km away) as well as the plume ages (up to 115 min) and was based on commercially available historical records of the Automatic Identification System. The dispersion lifetime of chemically inert C…

[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]Atmospheric Science010504 meteorology & atmospheric sciencesAtmospheric modelsParticle number020209 energy02 engineering and technologyParticulatesCombustionAtmospheric sciences01 natural scienceslcsh:QC1-999PlumeDilutionlcsh:Chemistrylcsh:QD1-99913. Climate action0202 electrical engineering electronic engineering information engineeringParticle14. Life underwaterlcsh:PhysicsNOx0105 earth and related environmental sciences
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Daytime formation of nitrous acid at a coastal remote site in Cyprus indicating a common ground source of atmospheric HONO and NO

2016

Characterization of daytime sources of nitrous acid (HONO) is crucial to understand atmospheric oxidation and radical cycling in the planetary boundary layer. HONO and numerous other atmospheric trace constituents were measured on the Mediterranean island of Cyprus during the CYPHEX (CYprus PHotochemical EXperiment) campaign in summer 2014. Average volume mixing ratios of HONO were 35 pptv (±25 pptv) with a HONO ∕ NOx ratio of 0.33, which was considerably higher than reported for most other rural and urban regions. Diel profiles of HONO showed peak values in the late morning (60 ± 28 pptv around 09:00 local time) and persistently high mixing ratios during daytime (45 ± 18 pptv), indicating …

lcsh:Chemistrylcsh:QD1-999lcsh:Physicslcsh:QC1-999Atmospheric Chemistry and Physics
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