Motivation
Observations of aerosol properties and meteorological conditions in
field campaigns all over the world
Instrument
Two seeded Nd:YAG lasers and two Titanium:Sapphire lasers emit light at
wavelengths of 1064, 800, 710, 532, 400 and 355 nm with an overall
power of twice 1.6 J and a repetition rate of 30 Hz. A 10-fold beam
expander reduces the beam divergence to less than 0.1
mrad. The backscattered light is collected with a 53-cm Cassegrain
telescope. A 14-channel receiver separates the
elastically backscattered signals at the six laser wavelengths and the
Raman signals of nitrogen at 387 and 607 nm and of water vapor at 660
nm by the use of dichroic
beamsplitters and interference filters. A polarizer discriminates the
parallel- and cross-polarized components of the 710-nm backscatter
signal. Two pure rotational Raman signals of nitrogen are separated by
a double-grating monochromator. All signals are detected with
photomultiplier
tubes and recorded in single-photon-counting mode or the
photomultiplier is operated in current mode.
From the detected signals, profiles of the backscatter coefficient at
the six emitted wavelengths, of the depolarization ratio, as well as
of the extinction coefficient and the lidar ratio at 355 and 532 nm are
determined. Furthermore,
profiles of water-vapor mixing ratio and temperature are derived. From
these two quantities the relative humidity can be determined in the
same scattering volume as the aerosol properties (Raman lidar
principle).
Setup
Cooperation
Implementation of the temperature channels (monochromator) by Yuri F.
Arshinov, Sergej M. Bobrovnikov, and Ilya B. Serikov from the Institute
for Atmospheric Optics, Siberian Branch of the Russian Acadamy of
Sciences, Tomsk, Russia
Projects