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@ARTICLE{Hirsikko:187194,
author = {Hirsikko, A. and O'Connor, E. J. and Komppula, M. and
Korhonen, K. and Pfüller, A. and Giannakaki, E. and Wood,
C. R. and Bauer-Pfundstein, M. and Poikonen, A. and
Karppinen, T. and Lonka, H. and Kurri, M. and Heinonen, J.
and Moisseev, D. and Asmi, E. and Aaltonen, V. and Nordbo,
A. and Rodriguez, E. and Lihavainen, H. and Laaksonen, A.
and Lehtinen, K. E. J. and Laurila, T. and Petäjä, T. and
Kulmala, M. and Viisanen, Y.},
title = {{O}bserving wind, aerosol particles, cloud and
precipitation: {F}inland's new ground-based remote-sensing
network},
journal = {Atmospheric measurement techniques},
volume = {7},
number = {5},
issn = {1867-8548},
address = {Katlenburg-Lindau},
publisher = {Copernicus},
reportid = {FZJ-2015-00868},
pages = {1351 - 1375},
year = {2014},
abstract = {The Finnish Meteorological Institute, in collaboration with
the University of Helsinki, has established a new
ground-based remote-sensing network in Finland. The network
consists of five topographically, ecologically and
climatically different sites distributed from southern to
northern Finland. The main goal of the network is to monitor
air pollution and boundary layer properties in near real
time, with a Doppler lidar and ceilometer at each site. In
addition to these operational tasks, two sites are members
of the Aerosols, Clouds and Trace gases Research
InfraStructure Network (ACTRIS); a Ka band cloud radar at
Sodankylä will provide cloud retrievals within CloudNet,
and a multi-wavelength Raman lidar, PollyXT (POrtabLe Lidar
sYstem eXTended), in Kuopio provides optical and
microphysical aerosol properties through EARLINET (the
European Aerosol Research Lidar Network). Three C-band
weather radars are located in the Helsinki metropolitan area
and are deployed for operational and research applications.
We performed two inter-comparison campaigns to investigate
the Doppler lidar performance, compare the backscatter
signal and wind profiles, and to optimize the lidar
sensitivity through adjusting the telescope focus length and
data-integration time to ensure sufficient signal-to-noise
ratio (SNR) in low-aerosol-content environments. In terms of
statistical characterization, the wind-profile comparison
showed good agreement between different lidars. Initially,
there was a discrepancy in the SNR and attenuated
backscatter coefficient profiles which arose from an
incorrectly reported telescope focus setting from one
instrument, together with the need to calibrate. After
diagnosing the true telescope focus length, calculating a
new attenuated backscatter coefficient profile with the new
telescope function and taking into account calibration, the
resulting attenuated backscatter profiles all showed good
agreement with each other. It was thought that harsh Finnish
winters could pose problems, but, due to the built-in
heating systems, low ambient temperatures had no, or only a
minor, impact on the lidar operation – including
scanning-head motion. However, accumulation of snow and ice
on the lens has been observed, which can lead to the
formation of a water/ice layer thus attenuating the signal
inconsistently. Thus, care must be taken to ensure
continuous snow removal.},
cin = {IEK-8},
ddc = {550},
cid = {I:(DE-Juel1)IEK-8-20101013},
pnm = {233 - Trace gas and aerosol processes in the troposphere
(POF2-233)},
pid = {G:(DE-HGF)POF2-233},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000336740700013},
doi = {10.5194/amt-7-1351-2014},
url = {https://juser.fz-juelich.de/record/187194},
}