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Relationships between IWC and Polarimetric Radar Measurands at 94 and 220 GHz for Hexagonal Columns and Plates

Relationships between IWC and Polarimetric Radar Measurands at 94 and 220 GHz for Hexagonal... Ice crystal models of a hexagonal column and hexagonal plate are used for deriving power-law relationships between ice water content (IWC) and various radar measurands, including Z h , K DP , A h , and Z DR (which are used together with Z h or K DP ) at 94- and 220-GHz frequencies. The scattering computations are performed with the finite-difference time-domain method. The IWC and radar measurands are simulated based on gamma model size distributions characteristic of cirrus clouds. All the relationships involving the polarimetric measurands K DP and Z DR have less than 15%% standard error (in the IWC estimate) when applied to the simulated size distributions. The standard errors for the IWC–– Z h and IWC–– A h relationships reach 40%%. These should be considered as lower limits to the errors resulting from the relationships. The biases increase with variations in the model ice crystal aspect ratio, density, and canting angle. The least affected relationships are those involving Z h and A h alone. Combining Z DR with Z h increases the biases compared to using only Z h . The largest biases from all of these relationships arise as a result of applying those for columns to plates and vice versa. This indicates the need for differentiating ice crystal types. The clustering of hexagonal columns and plates in different regions of the Z h –– Z DR and Z h –– K DP planes are suggested as a possible means of identifying them at side incidence, in addition to their depolarization signatures. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Atmospheric and Oceanic Technology American Meteorological Society

Relationships between IWC and Polarimetric Radar Measurands at 94 and 220 GHz for Hexagonal Columns and Plates

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Publisher
American Meteorological Society
Copyright
Copyright © 1996 American Meteorological Society
ISSN
1520-0426
DOI
10.1175/1520-0426(1997)014<1055:RBIAPR>2.0.CO;2
Publisher site
See Article on Publisher Site

Abstract

Ice crystal models of a hexagonal column and hexagonal plate are used for deriving power-law relationships between ice water content (IWC) and various radar measurands, including Z h , K DP , A h , and Z DR (which are used together with Z h or K DP ) at 94- and 220-GHz frequencies. The scattering computations are performed with the finite-difference time-domain method. The IWC and radar measurands are simulated based on gamma model size distributions characteristic of cirrus clouds. All the relationships involving the polarimetric measurands K DP and Z DR have less than 15%% standard error (in the IWC estimate) when applied to the simulated size distributions. The standard errors for the IWC–– Z h and IWC–– A h relationships reach 40%%. These should be considered as lower limits to the errors resulting from the relationships. The biases increase with variations in the model ice crystal aspect ratio, density, and canting angle. The least affected relationships are those involving Z h and A h alone. Combining Z DR with Z h increases the biases compared to using only Z h . The largest biases from all of these relationships arise as a result of applying those for columns to plates and vice versa. This indicates the need for differentiating ice crystal types. The clustering of hexagonal columns and plates in different regions of the Z h –– Z DR and Z h –– K DP planes are suggested as a possible means of identifying them at side incidence, in addition to their depolarization signatures.

Journal

Journal of Atmospheric and Oceanic TechnologyAmerican Meteorological Society

Published: Oct 30, 1996

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