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Sökning: WFRF:(O'Dowd C.) > Henzing B.

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1.
  • Wiedensohler, A., et al. (författare)
  • Mobility particle size spectrometers: harmonization of technical standards and data structure to facilitate high quality long-term observations of atmospheric particle number size distributions
  • 2012
  • Ingår i: Atmospheric Measurement Techniques. - Copernicus GmbH. - 1867-1381. ; 5:3, s. 657-685
  • Tidskriftsartikel (refereegranskat)abstract
    • Mobility particle size spectrometers often referred to as DMPS (Differential Mobility Particle Sizers) or SMPS (Scanning Mobility Particle Sizers) have found a wide range of applications in atmospheric aerosol research. However, comparability of measurements conducted world-wide is hampered by lack of generally accepted technical standards and guidelines with respect to the instrumental set-up, measurement mode, data evaluation as well as quality control. Technical standards were developed for a minimum requirement of mobility size spectrometry to perform long-term atmospheric aerosol measurements. Technical recommendations include continuous monitoring of flow rates, temperature, pressure, and relative humidity for the sheath and sample air in the differential mobility analyzer. We compared commercial and custom-made inversion routines to calculate the particle number size distributions from the measured electrical mobility distribution. All inversion routines are comparable within few per cent uncertainty for a given set of raw data. Furthermore, this work summarizes the results from several instrument intercomparison workshops conducted within the European infrastructure project EUSAAR (European Supersites for Atmospheric Aerosol Research) and ACTRIS (Aerosols, Clouds, and Trace gases Research InfraStructure Network) to determine present uncertainties especially of custom-built mobility particle size spectrometers. Under controlled laboratory conditions, the particle number size distributions from 20 to 200 nm determined by mobility particle size spectrometers of different design are within an uncertainty range of around +/- 10% after correcting internal particle losses, while below and above this size range the discrepancies increased. For particles larger than 200 nm, the uncertainty range increased to 30%, which could not be explained. The network reference mobility spectrometers with identical design agreed within +/- 4% in the peak particle number concentration when all settings were done carefully. The consistency of these reference instruments to the total particle number concentration was demonstrated to be less than 5%. Additionally, a new data structure for particle number size distributions was introduced to store and disseminate the data at EMEP (European Monitoring and Evaluation Program). This structure contains three levels: raw data, processed data, and final particle size distributions. Importantly, we recommend reporting raw measurements including all relevant instrument parameters as well as a complete documentation on all data transformation and correction steps. These technical and data structure standards aim to enhance the quality of long-term size distribution measurements, their comparability between different networks and sites, and their transparency and traceability back to raw data.
2.
  • Beddows, D. C. S., et al. (författare)
  • Variations in tropospheric submicron particle size distributions across the European continent 2008-2009
  • 2014
  • Ingår i: Atmospheric Chemistry and Physics. - Copernicus. - 1680-7316. ; 14:8, s. 4327-4348
  • Tidskriftsartikel (refereegranskat)abstract
    • Cluster analysis of particle number size distributions from background sites across Europe is presented. This generated a total of nine clusters of particle size distributions which could be further combined into two main groups, namely: a south-to-north category (four clusters) and a west-to-east category (five clusters). The first group was identified as most frequently being detected inside and around northern Germany and neighbouring countries, showing clear evidence of local afternoon nucleation and growth events that could be linked to movement of air masses from south to north arriving ultimately at the Arctic contributing to Arctic haze. The second group of particle size spectra proved to have narrower size distributions and collectively showed a dependence of modal diameter upon the longitude of the site (west to east) at which they were most frequently detected. These clusters indicated regional nucleation (at the coastal sites) growing to larger modes further inland. The apparent growth rate of the modal diameter was around 0.6-0.9 nm h(-1). Four specific air mass back-trajectories were successively taken as case studies to examine in real time the evolution of aerosol size distributions across Europe. While aerosol growth processes can be observed as aerosol traverses Europe, the processes are often obscured by the addition of aerosol by emissions en route. This study revealed that some of the 24 stations exhibit more complex behaviour than others, especially when impacted by local sources or a variety of different air masses. Overall, the aerosol size distribution clustering analysis greatly simplifies the complex data set and allows a description of aerosol aging processes, which reflects the longer-term average development of particle number size distributions as air masses advect across Europe.
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3.
  • Manninen, H. E., et al. (författare)
  • EUCAARI ion spectrometer measurements at 12 European sites - analysis of new particle formation events
  • 2010
  • Ingår i: Atmospheric Chemistry and Physics. - Copernicus GmbH. - 1680-7316. ; 10:16, s. 7907-7927
  • Tidskriftsartikel (refereegranskat)abstract
    • We present comprehensive results on continuous atmospheric cluster and particle measurements in the size range similar to 1-42 nm within the European Integrated project on Aerosol Cloud Climate and Air Quality interactions (EUCAARI) project. We focused on characterizing the spatial and temporal variation of new particle formation events and relevant particle formation parameters across Europe. Different types of air ion and cluster mobility spectrometers were deployed at 12 field sites across Europe from March 2008 to May 2009. The measurements were conducted in a wide variety of environments, including coastal and continental locations as well as sites at different altitudes (both in the boundary layer and the free troposphere). New particle formation events were detected at all of the 12 field sites during the year-long measurement period. From the data, nucleation and growth rates of newly formed particles were determined for each environment. In a case of parallel ion and neutral cluster measurements, we could also estimate the relative contribution of ion-induced and neutral nucleation to the total particle formation. The formation rates of charged particles at 2 nm accounted for 1-30% of the corresponding total particle formation rates. As a significant new result, we found out that the total particle formation rate varied much more between the different sites than the formation rate of charged particles. This work presents, so far, the most comprehensive effort to experimentally characterize nucleation and growth of atmospheric molecular clusters and nanoparticles at ground-based observation sites on a continental scale.
4.
  • Asmi, A., et al. (författare)
  • Number size distributions and seasonality of submicron particles in Europe 2008-2009
  • 2011
  • Ingår i: Atmospheric Chemistry and Physics. - Copernicus GmbH. - 1680-7316. ; 11:11, s. 5505-5538
  • Tidskriftsartikel (refereegranskat)abstract
    • Two years of harmonized aerosol number size distribution data from 24 European field monitoring sites have been analysed. The results give a comprehensive overview of the European near surface aerosol particle number concentrations and number size distributions between 30 and 500 nm of dry particle diameter. Spatial and temporal distribution of aerosols in the particle sizes most important for climate applications are presented. We also analyse the annual, weekly and diurnal cycles of the aerosol number concentrations, provide log-normal fitting parameters for median number size distributions, and give guidance notes for data users. Emphasis is placed on the usability of results within the aerosol modelling community.
5.
  • Hamburger, T., et al. (författare)
  • Overview of the synoptic and pollution situation over Europe during = e EUCAARI-LONGREX field campaign
  • 2011
  • Ingår i: Atmospheric Chemistry And Physics. - 1680-7316. ; 11:3, s. 1065-1082
  • Tidskriftsartikel (refereegranskat)abstract
    • In May 2008 the EUCAARI-LONGREX aircraft field campaign was conducted = thin the EUCAARI intensive observational period. The campaign aimed at = udying the distribution and evolution of air mass properties on a = ntinental scale. Airborne aerosol and trace gas measurements were = rformed aboard the German DLR Falcon 20 and the British FAAM B.4e-146 = rcraft. This paper outlines the meteorological situation over Europe = ring May 2008 and the temporal and spatial evolution of predominantly = thropogenic particulate pollution inside the boundary layer and the = ee troposphere. Time series data of six selected ground stations are = ed to discuss continuous measurements besides the single flights. The = servations encompass total and accumulation mode particle number = ncentration (0.1-0.8 mu m) and black carbon mass concentration as well = several meteorological parameters. Vertical profiles of total aerosol = mber concentration up to 10 km are compared to vertical profiles = obed during previous studies. During the first half of May 2008 an = ticyclonic blocking event dominated the weather over Central Europe. = led to increased pollutant concentrations within the centre of the = gh pressure inside the boundary layer. Due to long-range transport the = cumulated pollution was partly advected towards Western and Northern = rope. The measured aerosol number concentrations over Central Europe = owed in the boundary layer high values up to 14 000 cm(-3) for = rticles in diameter larger 10 nm and 2300 cm(-3) for accumulation mode = rticles during the high pressure period, whereas the middle free = oposphere showed rather low concentrations of particulates. Thus a = rong negative gradient of aerosol concentrations between the well = xed boundary layer and the clean middle troposphere occurred.
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