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Dual Polarization Lidar for Remote Sensing of Aerosols and Clouds in the Atmosphere


Affiliations
1 Centre of Studies in Resources Engineering, Indian Institute of Technology-Bombay, Powai, Mumbai 400 076, India
2 National Atmospheric Research Laboratory, Department of Space, Government of India, Gadanki 517 112, India
3 Photonics, Nuclear and Medical Physics Division, VIT University, Vellore 632 014, India
 

We describe an indigenously developed dual polarization lidar (DPL) system for remote sensing of the range resolved properties of non-spherical nature of air borne and cloud particles. The DPL system probes the atmosphere using a linearly polarized second harmoni cNd : YAG laser. The design of receiver optics is such that it separates the collected back scattered light into parallel and perpendicular polarization components.The ratio of intensity of perpendicular to parallel signals is known as the depolarization ratio (DR), which is a gauge for non-spherical particle content in the atmosphere. The DPL employs an external irradiance standard to calibrate the depolarization measurements.Comparison of simultaneous measurements between DPL and a similar instrument validates the utility of the system for cloud and aerosol studies. The altitude profiles of DR derived from lidar signals potentially indicate the type of major particle layers in the atmosphere.

Keywords

Aerosols, Clouds, Laser, Polarization Lidar, Remote Sensing.
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  • Sassen, K. and Benson, S., Ice nucleation in cirrus clouds: a model study of the homogeneous and heterogeneous mode. Geophys. Res. Lett., 2005, 27, 521–524.

  • Koepke, P. and Hess, M., Nonspherical particles and their influence on the scattering function of tropospheric aerosols. J. Aerosol Sci., 1986, 17(3), 254–257.

  • Lacis, A., Zhang, Y. C. and Rossow, W. B., Calculation of surface and top of atmosphere radiative fluxes from physical quantities based on ISCCP data sets 1. Method and sensitivity to input data uncertainties. J. Geophys. Res., 1995, 100, 1149–1165.

  • Liao, H. and Seinfeld, J. H., Radiative forcing by mineral dust aerosols: sensitivity to key variables. J. Geophys. Res., 1998, 103, 31637–31645.

  • Boucher, O. and Anderson, T. L. A., General circulation model assessment of the sensitivity of direct climate forcing by anthropogenic sulphate aerosols to aerosol size and chemistry. J. Geophys. Res., 1995, 100, 26117–26134.

  • Bhavani Kumar, Y., Lidar research activities and observations at NARL site, Gadanki, India. Proc. SPIE, 2016, 9879, 98790S.

  • Collis, R. T. H., Lidar for routine meteorological observations. Bull. Am. Meteorol. Soc., 1969, 50, 688–694.

  • Bhavani Kumar, Y., Portable lidar system for atmospheric boundary layer measurements. Opt. Eng., 2006, 45(7), 076201.

  • Sassen, K. and Cho, B. S., Subvisual-thin cirrus lidar dataset for satellite verification and climatological research. J. Appl. Meteorol. 1992, 31, 1275–1285.

  • Hunt, W. H., Winker, D. M., Vaughan, M. A., Powell, K. A., Lucker, P. L. and Weimer, C., CALIPSO Lidar description and performance assessment. J. Atmos. Ocean. Technol., 2009, 26, 1214–1228.

  • Murayama, T., Okamoto, H., Kaneyasu, N., Kamataki, H. and Miura, K., Application of lidar depolarization measurement in the atmospheric boundary layer: effects of dust and sea-salt particles. J. Geophys. Res., 1999, 104(D24), 31781–31792.

  • Sugimoto, N. et al., Record heavy Asian dust in Beijing in 2002: observations and model analysis of recent events. Geophys. Res. Lett., 2003, 30(12), 1640; doi: 10.1029/2002GL016349.

  • Ansmann, A. et al., Long range transport of Saharan dust to northern Europe: the 11–16 October 2001 ourtbreak observed with EARLINET. J. Geophys. Res., 2003, 108(D24), 4783, doi:10.1029/2003JD003757.

  • Shimizu, A. et al., Continuous observations of Asian dust and other aerosols by polarization lidar in China and Japan during ACE-Asia. J. Geophys. Res., 2004, 109, D19S17; doi:10.1029/2002JD003253.

  • Sassen, K., The polarization lidar technique for cloud research: a review and current assessment. Bull. Am. Meteorol. Soc., 1991, 72, 1848–1866.


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  • Dual Polarization Lidar for Remote Sensing of Aerosols and Clouds in the Atmosphere

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Authors

Ajay Kumar Patel
Centre of Studies in Resources Engineering, Indian Institute of Technology-Bombay, Powai, Mumbai 400 076, India
Bhavani Kumar Yellapragada
Centre of Studies in Resources Engineering, Indian Institute of Technology-Bombay, Powai, Mumbai 400 076, India
R. Vishnu
National Atmospheric Research Laboratory, Department of Space, Government of India, Gadanki 517 112, India
M. V. R. Murti
Centre of Studies in Resources Engineering, Indian Institute of Technology-Bombay, Powai, Mumbai 400 076, India
James Jebaseelan Samuel
Photonics, Nuclear and Medical Physics Division, VIT University, Vellore 632 014, India

Abstract


We describe an indigenously developed dual polarization lidar (DPL) system for remote sensing of the range resolved properties of non-spherical nature of air borne and cloud particles. The DPL system probes the atmosphere using a linearly polarized second harmoni cNd : YAG laser. The design of receiver optics is such that it separates the collected back scattered light into parallel and perpendicular polarization components.The ratio of intensity of perpendicular to parallel signals is known as the depolarization ratio (DR), which is a gauge for non-spherical particle content in the atmosphere. The DPL employs an external irradiance standard to calibrate the depolarization measurements.Comparison of simultaneous measurements between DPL and a similar instrument validates the utility of the system for cloud and aerosol studies. The altitude profiles of DR derived from lidar signals potentially indicate the type of major particle layers in the atmosphere.

Keywords


Aerosols, Clouds, Laser, Polarization Lidar, Remote Sensing.

References





DOI: https://doi.org/10.18520/cs%2Fv113%2Fi06%2F1134-1138