EARLINET:
long term observations for aerosol study
L. Mona1, U. Wandinger2, H.
Linnè3, A. Amodeo1, A. Apituley4, L. Alados
Arboledas5, D. Balis6, A. Chaikovsky7, A.
Comeron8, V. Freudenthaler9, I. Grigorov10, O.
Gustafsson11, S. Kinne3, D. Nicolae12, I. Mattis2,
V. Mitev13, A. Papayannis14, M.R. Perrone15,
A. Pietruczuk16, M.Pujadas17, J.P. Putaud18,
F. Ravetta19, V. Rizi20, V. Simeonov21, N.
Spinelli22, K. Stebel23, T. Trickl24, M. Wiegner9, G.Pappalardo1
1Istituto di Metodologie per
l’Analisi Ambientale CNR-IMAA, Potenza, I-85050, Italy pappalardo@imaa.cnr.it
2Institut für Troposphärenforschung,
Leipzig, Germany
3Max-Planck-Institut für Meteorologie,
Hamburg, Germany
4Rijksinstituut voor Volksgezondheid en
Milieu, Bilthoven, The Netherlands
5Universidad de Granada, Granada, Spain
6Aristoteleio Panepistimio, Thessalonikis, Greece
7Institute of Physics, National Academy of
Sciences, Minsk, Bjelarus
8Universitat Politècnica de Catalunya, Barcelona,
Spain
9Ludwig-Maximilians-Universität, München, Germany
10Institute of Electronics, Bulgarian Academy of
Sciences, Sofia, Bulgaria
11Swedish Defence Research Agency (FOI),
Linköping, Sweden
12National Institute of R&D for
Optoelectronics, Magurele-Bucharest, Romania
13CSEM, Centre Suisse
d'Electronique et de Microtechnique SA, Neuchâtel, Switzerland
14National Technical University of Athens,
Department of Physics, Athens, Greece
15Università del Salento, Department of Physics,
Lecce, Italy
16Institute of Geophysics, Polish Academy of
Sciences, Warsaw, Poland
17Centro de Investigaciones
Energéticas, Medioambientales y Tecnológicas, Madrid, Spain
18EC Joint Research Centre,
Ispra (VA), Italy
19Université Pierre et Maris
Curie-Institut Pierre Simon Laplace, Paris, France
20Università degli Studi
dell’Aquila - Dipartimento di Fisica - CETEMPS, L’Aquila, Italy
21Ecole Polytechnique Fédérale
de Lausanne, Switzerland
22Consorzio Nazionale
Interuniversitario per le Scienze Fisiche della Materia, Napoli, Italy
23Norwegian Institute for Air Research (NILU),
Kjeller, Norway
24Forschungszentrum Karlsruhe IMK-IFU,
Garmisch-Partenkirchen, Germany
The last IPCC
scientific report (Forster et al., 2007) underlines that it is not actually
possible to draw a conclusion about the effect of human activities on radiation
budget because of the high uncertainty about aerosol direct and indirect
effects. More observations, and in particular altitude resolved measurements,
are needed in order to further reduce this uncertainty. Lidar techniques allow
direct measurements of aerosol extinction (and therefore of the optical depth)
without critical assumptions and allow the description of the aerosol vertical
distribution. Therefore lidar measurements are an indispensable tool to study
the vertical structure of aerosol field and to investigate aerosol optical
properties. In order to study aerosol on large spatial scale and to investigate
transport and modification phenomena taking into account the vertical mixing
processes, observations performed by lidar networks are essentially needed.
These are the motivations why EARLINET, the European Aerosol Research Lidar
Network, was established in 2000, as a research program funded by the European
Commission in the frame of the 5th framework program. After the end of the
project, the network activity continued on the base of a voluntary association.
On March 2006, the EC Project EARLINET-ASOS (Advanced Sustainable Observation
System http://www.earlinetasos.org) started on
the base of the EARLINET infrastructure. This infrastructure project will
enhance the operation of the network.
At present, EARLINET consists of 25 lidar
stations: 7 single backscatter lidar stations, 9 Raman lidar stations with the
UV Raman channel for independent measurements of aerosol extinction and
backscatter, and 9 multi-wavelength Raman lidar stations.
A long-term database of aerosol lidar
measurements is collected within EARLINET since May 2000. In particular,
measurement are performed, almost simultaneously by all EARLINET stations, 3
times per week following a regular schedule established within the network
(Bosenberg et al., 2003). In addition to the
routine measurements, further observations are devoted to monitor special
events such as Saharan dust outbreaks, forest fires, photochemical smog and
volcano eruptions.
Data quality is assured by
intercomparisons of both instruments and retrieval algorithms for backscatter
and Raman lidar data. Moreover, tools for the continuous quality check of the
instruments and algorithms used have been developed within the network in order
to assure that data provided within EARLINET are always of the highest possible
quality level.
Thanks to the large amount of high
quality data, EARLINET database can contribute significantly to the
quantification of aerosol concentrations, radiative properties, long-range
transport and budget, and prediction of future trends on European and global
scale. It can also contribute to improve model treatment on a wide range of
scales and to a better exploitation of present and future satellite data.
However, an accurate quantification of
aerosol and cloud radiative forcing requires a synergistic approach of
satellite and ground-based observations together with model calculations. In
this context, EARLINET consortium is exploring possibilities about scientific
study based on the integration with different datasets, like AERONET and EMEP
data.
Moreover, since
June 2006, EARLINET is involved in the validation and exploitation of lidar data provided within the CALIPSO
(Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations) mission
(Mona et al., 2009; Pappalardo et al., 2009). This satellite mission provides a
first unique opportunity to address the study the 4-dimensional distribution of
aerosols and clouds on a global scale. Because of its geographic coverage and
its high quality, the EARLINET network is an optimal instrument to increase and
validate the accuracy of aerosol optical properties retrieved from the CALIPSO
pure backscatter lidar, and to investigate the representativeness of CALIPSO
observations.
Finally, EARLINET
data will be used for aerosol models validation. First systematic quantitative
comparisons with the DREAM (Dust REgional Atmospheric Model) dust forecast
model have been carried out for selected stations with large number of dust
observations.
The financial
support by the European Commission for EARLINET (grant RICA-025991) and through
GEOmon Integrated Project under the 6th Framework Programme (contract number
FP6-2005-Global-4-036677) is gratefully acknowledged.
Bösenberg, J., V. Matthias, A. Amodeo, et al., (2003) EARLINET: A
European Aerosol Research Lidar Network to Establish an Aerosol Climatology.
Max-Planck-Institut Report No. 348.
Forster, P., et al.
(2007), in Climate Change 2007: The Physical Science Basis, edited by S.
Solomon, D. Qin, M. Manning, Z. Chen, M. Marquis, K. B. Averyt, M. Tignor, and
H. L. Miller, Cambridge Univ. Press, New York.
Mona, L., et al.
(2009), One year of CNR-IMAA multi-wavelength Raman lidar measurements in
coincidence with CALIPSO overpasses: Level 1 products comparison, in press on
Atmos. Chem. And Phys.
Pappalardo, G., et
al. (2009), EARLINET correlative measurements for CALIPSO: first intercomparison
results, submitted to Jour. Geo. Res.