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The depolarization - attenuated backscatter relation: CALIPSO lidar measurements vs. theory
Author(s) -
Yongxiang Hu,
Mark Vaughan,
Zhaoyan Liu,
Bing Lin,
Ping Yang,
D. E. Flittner,
Bill Hunt,
Ralph E. Kuehn,
Jianping Huang,
Dong Wu,
Sharon Rodier,
Kathy Powell,
Charles R. Trepte,
David M. Winker
Publication year - 2007
Publication title -
optics express
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.394
H-Index - 271
ISSN - 1094-4087
DOI - 10.1364/oe.15.005327
Subject(s) - lidar , backscatter (email) , depolarization ratio , aerosol , depolarization , satellite , optics , remote sensing , mie scattering , pathfinder , ice crystals , atmospheric sciences , monte carlo method , environmental science , materials science , scattering , physics , meteorology , light scattering , geology , astronomy , medicine , telecommunications , statistics , mathematics , computer science , library science , wireless , endocrinology
Using measurements obtained by the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) satellite, relationships between layer-integrated depolarization ratio (delta) and layer-integrated attenuated backscatter (gamma) are established for moderately thick clouds of both ice and water. A new and simple form of the delta-gamma relation for spherical particles, developed from Monte Carlo simulations and suitable for both water clouds and spherical aerosol particles, is found to agree well with the observations. A high-backscatter, low-depolarization delta-gamma relationship observed for some ice clouds is shown to result primarily from horizontally oriented plates and implies a preferential lidar ratio - depolarization ratio relation in nature for ice cloud particles containing plates.

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