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Scattering And Absorption of Light in Planetary Regoliths
Published on: July 1, 2019
Optical backscattering from near-spherical water, ice, and mixed phase drops
Applied Optics
|February 20, 2010
Summary
This study examined how artificial raindrops scatter laser light in ice and mixed phases. Results show distinct scattering patterns for liquid drops, frozen drops, and during phase transitions, aiding lidar measurements of atmospheric ice particles.
Area of Science:
- Atmospheric optics
- Cloud physics
- Laser scattering
Background:
- Understanding hydrometeor scattering is crucial for remote sensing.
- Previous studies have limitations in characterizing phase-dependent scattering.
Purpose of the Study:
- To experimentally assess the scattering behavior of artificial raindrops in ice and mixed phases.
- To investigate the influence of drop shape and phase transitions on light depolarization.
- To relate scattering properties to lidar measurements of atmospheric particles.
Main Methods:
- Simultaneous measurement of parallel and cross-polarized backscattered laser light (6328 Å).
- Experimental setup using freely falling and mechanically suspended artificial drops.
- Analysis of linear depolarization ratios (delta) across different drop states.
Main Results:
- Depolarization ratios (delta) were <0.01 for liquid drops, ~0.5 for regular ice, and 0.35-1.0 for irregular ice.
- Anomalous scattering (delta > 1.0) observed during liquid-to-solid phase transition.
- Significant parallel polarized energy returned from larger raindrops (>~4 mm).
- Melting ice drops maintained ice-like depolarization until most ice had transformed.
Conclusions:
- Scattering behavior varies significantly with hydrometeor phase and shape.
- Observed phenomena provide insights into scattering mechanisms of large, near-spherical particles.
- Findings have implications for interpreting lidar data of atmospheric hydrometeors.

