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Microphysical particle parameters from extinction and backscatter lidar data by inversion with regularization:

D Müller1, U Wandinger, A Ansmann

  • 1Institute for Tropospheric Research, Permoserstrasse 15, 04318 Leipzig, Germany. detlef@tropos.de

Applied Optics
|March 6, 2008
PubMed
Summary
This summary is machine-generated.

This study introduces a new method to determine tropospheric particle properties from lidar measurements. The technique accurately retrieves particle size distribution parameters and refractive index, crucial for atmospheric research.

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Area of Science:

  • Atmospheric Science
  • Lidar Remote Sensing
  • Aerosol Physics

Background:

  • Accurate characterization of tropospheric particle size distributions is essential for understanding aerosol impacts on climate and air quality.
  • Current methods often rely on assumptions about particle shape or require extensive datasets, limiting routine application.

Purpose of the Study:

  • To develop and validate a robust method for retrieving physical parameters of tropospheric particle size distributions from multi-wavelength lidar data.
  • To assess the accuracy and limitations of the proposed inversion algorithm for routine atmospheric profiling.

Main Methods:

  • Utilized multi-wavelength lidar measurements (355-1064 nm for backscatter, 355 & 532 nm for extinction).
  • Employed an inversion algorithm with generalized cross-validation for regularization.
  • The method does not assume particle size distribution shape and accommodates up to 20% measurement errors.

Main Results:

  • Successfully retrieved effective radius, volume, and surface-area concentrations with +/-50% accuracy.
  • Determined the real part of the complex refractive index to +/-0.05 and the imaginary part to +/-50%.
  • Demonstrated the necessity of at least two extinction wavelengths for accurate parameter retrieval.

Conclusions:

  • The proposed inversion method provides a reliable approach for routine retrieval of key aerosol physical properties from lidar data.
  • The method's ability to handle measurement errors and distributional shape assumptions enhances its practical applicability in atmospheric studies.
  • While effective radius, volume, and surface-area concentrations are retrieved with reasonable accuracy, number concentrations may exhibit larger uncertainties.