Aerosol Classification by Simultaneous
Star-Photometer and Raman Lidar Measurements
D. Kaiser1, V. Novikov2,
D. Müller3, U. Leiterer4, F. Immler1 and O.
Schrems1
1 Alfred-Wegener-Institute for Polar and Marine Research,
Bremerhaven, Germany
2 Central Astronomical Observatory of the Russian Academy of
Sciences, Pulkovo, Russia
3 Institute for Tropospheric Research, Leipzig, Germany
4 Meteorological Observatory Lindenberg of the German Weather
Service, Lindenberg, Germany
03.06.2005, 13.00 c.t.
Room S3120
Aerosol Particles (AP) are one of the largest uncertainties in climate
forcing assessment. Highly variable concentrations in the atmosphere and
numerous types of AP make the monitoring of the atmospheric aerosol a difficult
problem. In-situ measurements are very reliable but do in general not provide
the total optical depth. Satellite measurements provide global coverage but have
a limited scope and accuracy.
Ground-based measurements with Photometer and Lidar deliver total column
(Photometer) and profile (Lidar) aerosol optical properties, which allow for the
derivation of size distribution, refractive index, scattering function and
Single Scattering Albedo. The inversion algorithms have been compared to in-situ
measurements in some single cases and shown good agreement (Masonis 2002, Müller
2001).
Star-Photometer and Raman Lidar measurements have been made simultaneously
during the measurement campaigns MARL@MOL2003 and LITFASS2003 in Lindenberg,
Germany from May to September 2003. The spectral resolution of the
star-photometer (9 wavelengths) and Raman Lidar extinction, backscatter and
depolarisation profiles allow for an extended characterisation of AP.
Extinction coefficients can not be measured from the ground, as emitted
laser beam and telescope field-of-view do not overlap completely. A calculation
of the exact overlap function has been made ("overlap correction") to extend the
range of extinction profiles down to 2 km above the ground depending on
atmospheric conditions. The total OD including the 2 lowermost km of the
atmospheric aerosol can by measured with Star-Photometer.
Optical and Microphysical Properties of three days are analysed at
different altitudes. A comparison of the two instruments shows good agreement in
many cases. Star-Photometer and Raman Lidar (SPLI) can be fruitfully combined to
study AP.