z-logo
open-access-imgOpen Access
Layers of quasi-horizontally oriented ice crystals in cirrus clouds observed by a two-wavelength polarization lidar
Author(s) -
Anatoli G. Borovoi,
Yu. S. Balin,
Grigorii Kokhanenko,
Ioganes E. Penner,
Alexander V. Konoshonkin,
Natalia V. Kustova
Publication year - 2014
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.22.024566
Subject(s) - cirrus , lidar , optics , wavelength , polarization (electrochemistry) , ice crystals , depolarization ratio , materials science , atmospheric optics , backscatter (email) , ice cloud , remote sensing , physics , geology , radiative transfer , telecommunications , chemistry , computer science , wireless
Layers of quasi-horizontally oriented ice crystals in cirrus clouds are observed by a two-wavelength polarization lidar. These layers of thickness of several hundred meters are identified by three attributes: the backscatter reveals a sharp ridge while the depolarization ratio and color ratio become deep minima. These attributes have been justified by theoretical calculations of these quantities within the framework of the physical-optics approximation.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here