Physics Department

Research Group
"Optical Remote Measurements - Analysis of Atmospheric Processes with Optical Methods"


Six-Wavelength Lidar


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


Just click on picture to enlarge!
Six-wavelength aerosol lidar
(for field campaigns)


Take a little tour by clicking on the pictures!

Ramanlidar Container from Outside Lidar Emitter: Titan-Saphire Lasers Lidar Emitter: Titan-Saphire Lasers with optics

Separation of backscattered light:
  • elastic signals at 355, 400, 532, 710, 800, and 1064 nm
  • vibration-rotation Raman signals of nitrogen at 387 and 607 nm
  • vibration-rotation Raman signals of water vapor at 660 nm
  • pure rotational Raman signals at 532 nm
  • parallel- and cross-polarized components of the 710-nm signal


Take a little tour by clicking on the pictures!

Lidar Inside Ramalidar Seperation 1
Ramalidar Seperation 2 Ramalidar Seperation 3

Separation of two rotational Raman signals with a double-grating monochromator for temperature measurement

Arrangement of optical fibers in the monofiber blocks of the double-grating monochromator

Derived parameters:
  • Extinction coefficient at 355 and 532 nm
  • Depolarization ratio at 710 nm
  • Backscatter coefficient at 355, 400, 532, 710, 800, and 1064 nm
  • Lidar ratio at 355 and 532 nm
  • Temperature
  • Water-vapor mixing ratio
  • Relative humidity

top of page  


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



Publications

Althausen, D., Müller, D., Ansmann, A., Wandinger, U., Hube, H., Clauder, E. and Zörner, S. 2000. Scanning 6-wavelength 11-channel aerosol lidar. J. Atmos. Ocean. Tech., 17, 1469-1482.

top of page

Last modification: 2005-12-21