Technical note
A novel approach for the characterization of transport and optical properties of aerosol particles near sources – Part I: Measurement of particle backscatter coefficient maps with a scanning UV lidar

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Abstract

The physical and chemical properties of aerosols emitted from a livestock farm were determined by a novel approach which combines high-resolution lidar measurements (0.33 s, 30 m) with simulations of a microphysics–chemistry–transport model. This first of two companion papers describes the scanning lidar measurements of optical particle properties. The lidar system employed laser radiation at a wavelength of 355 nm with a power of 9 W and a pulse repetition rate of 30 Hz. The laser beam was expanded before transmission to the atmosphere so that it became eye-safe at distances >270 m to the lidar. The elastic backscatter signal was detected with a resolution of 0.033 s and 3 m. A receiving telescope with a primary-mirror diameter of 40 cm was used. For this system, we developed a novel method for two-dimensional retrievals of the particle backscatter coefficient. With this set up and approach, the lidar was able to identify the aerosol plume up to a range of ∼2.5 km from the source, a farm in northern Germany, in daytime. The measurements confirm that the optical particle properties of the emission plume vary largely with distance from the source and that the maximum particle backscatter coefficient is found away from the source. Within a close-to-horizontal scan (elevation angle of 2.3°), we found a mean particle backscatter coefficient of 1.5·10−5 m−1 sr−1 inside the plume between 1.5 and 2.0 km distance from the source. Subtraction of the mean particle backscatter coefficient of the background aerosol present in this case (4.1·10−6 m−1 sr−1) yields a particle backscatter coefficient of the livestock aerosols of 1.1·10−5 m−1 sr−1. The limited extend of the plume is revealed with the scanning lidar: Scans with a slightly higher elevation angle of 4.8° did not pick up the plume.

Introduction

The impact of livestock facilities on the environment, especially in areas with dense animal populations, can become significant (e.g., Denby et al., 2008). Livestock farm emissions are partly particulate matter and partly gaseous. The emitted gases, like, e.g., ammonia, are partly aerosol precursors, so that the farm emissions contribute directly and indirectly to the aerosol load in the environment (Lammel et al., 2004, Lammel et al., 2005). The emissions pose a hazard to the health of the inhabitants surrounding the sources and to the farmers working at the facilities (e.g., Cambra-López et al., 2010). Furthermore, aerosol particles from livestock farm emissions contribute to the effect of aerosols on anthropogenic climate change. The uncertainty of this contribution is still large (IPCC, 2007). The experimental quantification of the aerosol emission from livestock facilities is a prerequisite to characterise the potential impact of these particles. Little is known, about their optical properties which, however, is an important aspect for assessing their climate impact. A complicating fact in this context is that livestock aerosol properties are undergoing rapid changes close to their sources that affect the composition of particles far away from the source (Lammel et al., 2005).

So far only a few studies on aerosols originating from livestock buildings exist. Some research efforts have been performed to investigate the aerosol emissions of livestock farming using point measurements around the facilities. Takai et al. (1998) made field surveys of indoor dust concentrations and dust emissions from various farms with cattle and poultry. Lammel et al. (2004) investigated the constituents of the aerosols emitted from a livestock facility in southern Germany with ground measurements collected downwind and upwind of the farm. Some studies exist on the yearly or monthly amount of emission (e.g. Costa and Guarino, 2009). But no study allowed yet for volume integrated mass budgeting because of the limitations the experimental studies based on point measurements have: (1) they cannot adequately provide the spatial and temporal distribution of plumes, (2) they cannot resolve the transport processes under different environmental conditions, (3) emissions from the farms are not continuous and thus measurements at certain times give erroneous results in case of varying emission rates. As a result, our knowledge is still insufficient to describe the spatial extent and the transformation during the transport of livestock aerosols in order to assess their significance.

This problem calls for the application of remote sensing techniques: Lidar can determine the range-resolved distributions of optical properties of atmospheric aerosols with high temporal and spatial resolution up to a range of several kilometers (see, e.g., Weitkamp, 2005 for an overview of the lidar technique). In order to investigate the spatial distribution of aerosol particles, scanning lidars can be applied (e.g., Piironen and Eloranta, 1995, Mayor and Spuler, 2004).

While lidar has been used for a large number of other atmospheric studies, only a few lidar studies on livestock aerosols have been reported to date. Hartung et al. (1998) characterised the aerosol emission from a farm by tilling and reported an increase of the backscatter signal intensity in one profile. The transformations of aerosol properties during transport could not be addressed, partly because of the restrictions for operation of their non-eye-safe lidar. Prueger et al. (2008) investigated the dispersion of particulate matter outside an animal husbandry by means of eddy covariance on towers and supported their findings with scanning elastic lidar measurements that detected the transport of the plume. Both studies did not quantify optical properties of the aerosols.

In this study, we employ the scanning aerosol lidar system of the University of Hohenheim (UHOH) that emits laser pulses with a wavelength of 355 nm with 30 Hz and 9 W average power. The use of the frequency-tripled ND:YAG laser radiation compared to the frequency-doubled or fundamental Nd:YAG laser radiation has two main advantages: (1) eye-safety for higher laser power and (2) the possibility to calibrate the lidar measurements with the strong molecular backscatter signal in the UV and to derive therefore the particle backscatter coefficient at the laser wavelength with the method based on Fernald (1984). Larger laser light intensity is also uncritical for the eye at wavelengths around 1.5 μm. To reach this wavelength range, however, special lasers have to be developed as transmitters for aerosol lidar (Spuler and Mayor, 2007, Petrova-Mayor et al., 2008). Furthermore, the Rayleigh backscatter cross section is a factor of (1500/355)4 = 319 weaker at 1.5 μm compared to 355 nm which is a disadvantage for calibrating the data. At the time of this experiment, the UHOH lidar detected only the elastic backscatter signal. Later, rotational Raman channels were added (Radlach et al., 2008) to the system that allow the independent measurement of the particle backscatter coefficient and the particle extinction coefficient (Behrendt et al., 2002) as well as temperature measurements (Behrendt, 2005, Groenemeijer et al., 2009, Radlach, 2009, Behrendt et al., 2010).

To allow for volume integrated mass budgeting, our lidar measurements were combined with in-situ measurements and large-eddy-simulation modelling within a collaborative project of UHOH and Max Planck Institute of Meteorology. The field campaign (hereafter named PLUS1 campaign) was conducted in the framework of the BW-PLUS (Baden-Württemberg Programm Lebensgrundlage Umwelt and ihre Sicherung) programme. This paper, the first of the two parts, provides a description of the UHOH scanning lidar system and discusses the technique to derive the particle backscatter coefficient. In a companion paper (Valdebenito et al., 2011), results obtained with the UHOH scanning lidar and with a high-resolution atmosphere–microphysics–chemistry model are combined.

This paper is organised as follows: Technical details of the UHOH scanning lidar system are presented in Section 2. A description of the lidar data analysis technique is given in Section 3. An overview of the lidar results of the PLUS1 campaign is given in Section 4. The combination of the lidar measurements with results of a large-eddy-simulation aerosol-optical-property model are outlined in Section 5. A summary and an outlook are given in Section 6.

Section snippets

Set-up of the scanning lidar

Fig. 1 shows a scheme of the scanning lidar of University of Hohenheim. The whole system is mounted in a truck so that it can be transported for field deployments. A flash-lamp-pumped frequency-tripled Nd:YAG laser (GCR5-30 of Spectra-Physics) with a pulse repetition rate of 30 Hz and a pulse energy of ∼300 mJ at a wavelength of 355 nm is used as laser transmitter. The pulse length is 5 ns. The radiation at 355 nm is separated from radiation at 1064 and 532 nm (primary and secondary Nd:YAG

Technique to determine the backscatter coefficient

The elastic-backscatter signal at 355 nm allows for measurements of the backscatter coefficient by analytical inversion of the lidar equation (Fernald, 1984). In practice, the backscatter signals P(r) are measured at discrete ranges r and the backscatter coefficient can be calculated stepwise with step length Δr (equal to the range resolution of the data) viaβ(rΔr)=I(rΔr)exp[(SparSmol)(βmol(rΔr)+βmol(r))Δr]I(r)β(r)Spar(I(r)+I(rΔr)exp[(SparSmol)(βmol(rΔr)+βmol(r))Δr])Δrwith I(r)=P(r)r2

Particle backscatter coefficient mapping of livestock aerosols

The PLUS1 campaign took place from 11 to 21 September 2005 in close vicinity of a livestock farm (52°19.44′ N; 7°8.8′ E; 56 m above sea level) in Mettingen, northern Germany. The ground distance between the farm and lidar was 480 m with the farm situated at an azimuth angle of 193.5° (measured from the geographical north) from the lidar position. The livestock facility hosted 1800 pigs and was actively ventilated from two chimneys separated by about 30 m from each other with output of 9 ± 2 m3s

Combination of lidar measurements and large-eddy-simulation aerosol-optical-property model

The high-resolution lidar measurements obtained with the scanning UV lidar have been combined with high-resolution atmosphere–microphysics–chemistry model simulations to analyse the aerosol transformation during transport on a small spatial and temporal scale (Valdebenito et al., 2011). In-situ point measurements served for the characterisation of physical and chemical properties of the aerosols surrounding the source. On the basis of these measurements, the large-eddy-simulation

Summary and conclusions

A new mobile eye-safe scanning aerosol lidar at 355 nm has been developed at UHOH to derive information on spatial distribution and optical property of aerosol particles in the lower troposphere. The lidar system was operated with an average power of 9 W in combination with a 40-cm scanner with a scan speed of up to 10° s−1. A two-dimensional retrieval technique was developed for determining particle backscatter coefficient maps with resolutions in the order of a few meters. It is based on an

Acknowledgements

This project work was conducted in the framework of the BW-PLUS programme, funded by the Ministry of the Environment and Transport of the state of Baden-Württemberg, Germany. We thank Marcus Radlach (UHOH) for his help during the development of the lidar system as well as during the PLUS1 campaign. We highly appreciate the support of GKSS Research Centre, Germany, for donating the mobile platform and our colleagues at NCAR, USA, for building the scanner. Finally, we would like to thank three

References (42)

  • A. Behrendt et al.

    3-dimensional observations of atmospheric humidity with a scanning differential absorption lidar. Remote sensing of clouds and the atmosphere XIV

  • A. Behrendt et al.

    Observation of convection initiation processes with a suite of state-of-the-art research instruments during COPS IOP8b

    Quartely Journal of Royal Meteorology Society.

    (2010)
  • L.R. Bissonnette

    Sensitivity analysis of lidar inversion algorithms

    Applied Optics

    (1986)
  • A. Bucholtz

    Rayleigh-scattering calculations for the terrestrial atmosphere

    Applied Optics

    (1995)
  • G.F. Fernald

    Determination of aerosol height distribution by lidar

    Applied Optics

    (1984)
  • M. Grzeschik et al.

    Four-dimensional variational analysis of water-vapor Raman lidar data and their impact on mesoscale forecasts

    Journal of Atmospheric and Oceanic Technology

    (2008)
  • P. Groenemeijer et al.

    Multi-sensor measurements of a convective storm cluster over a low mountain range: adaptive observations during PRINCE

    Monthly Weather Review

    (2009)
  • J. Hartung et al.

    Emission and distribution of particulates from a piggery with a central air exhaust

    Deutsche Tierärztliche Wochenschrift

    (1998)
  • IIASA

    Rains PM Module

    (2001)
  • IPCC

    Climate change 2007: the physical science basis

  • V.A. Kovalev

    Sensitivity of the lidar solution to errors of the aerosol backscatter-to-extinction ratio: influence of a monotonic change in the aerosol extinction coefficient

    Applied Optics

    (1995)
  • Cited by (0)

    1

    Present address: Laboratoire des Sciences du Climat et de l’Environnement (LSCE), Gif-Sur-Yvette, France.

    2

    Present address: Norwegian Meteorological Institute, Oslo, Norway.

    3

    Present address: Max Planck Institute for Chemistry, Mainz, Germany.

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