Editorial Type:
Article
Article Type:
Research Article

Linear Depolarization Ratios of Columnar Ice Crystals in a Deep Precipitating System over the Arctic Observed by Zenith-Pointing Ka-Band Doppler Radar

Mariko Oue Department of Meteorology, The Pennsylvania State University, University Park, Pennsylvania

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Matthew R. Kumjian Department of Meteorology, The Pennsylvania State University, University Park, Pennsylvania

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Yinghui Lu Department of Meteorology, and Department of Electrical Engineering, The Pennsylvania State University, University Park, Pennsylvania

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Johannes Verlinde Department of Meteorology, The Pennsylvania State University, University Park, Pennsylvania

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Kultegin Aydin Department of Electrical Engineering, The Pennsylvania State University, University Park, Pennsylvania

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Eugene E. Clothiaux Department of Meteorology, The Pennsylvania State University, University Park, Pennsylvania

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Print Publication:
01 May 2015
DOI:
https://doi.org/10.1175/JAMC-D-15-0012.1
Page(s):
1060–1068
Restricted access

Abstract

This study demonstrates that linear depolarization ratio (LDR) values obtained from zenith-pointing Ka-band radar Doppler velocity spectra are sufficient for detecting columnar ice crystals. During a deep precipitating system over the Arctic on 7 December 2013, the radar recorded LDR values up to −15 dB at temperatures corresponding to the columnar ice crystal growth regime. These LDR values were also consistent with scattering calculations for columnar ice crystals. Enhancements in LDR were suppressed within precipitation fallstreaks because the enhanced LDR values of columnar ice crystals were masked by the returns from the particles within the fallstreaks. However, Doppler velocity spectra of LDR within the fallstreak distinguished populations of slower-falling particles with high LDR (>−15 dB) and faster-falling particles with much lower LDR, suggesting that columnar ice crystals with high LDR coexisted with larger isometric particles that produced low LDR while dominating the total copolar reflectivity, thereby decreasing LDR. The measurements suggest that the columnar ice crystals originated in liquid-cloud layers through secondary ice production.

Corresponding author address: Mariko Oue, Dept. of Meteorology, The Pennsylvania State University, University Park, PA 16802. E-mail: muo15@psu.edu

Abstract

This study demonstrates that linear depolarization ratio (LDR) values obtained from zenith-pointing Ka-band radar Doppler velocity spectra are sufficient for detecting columnar ice crystals. During a deep precipitating system over the Arctic on 7 December 2013, the radar recorded LDR values up to −15 dB at temperatures corresponding to the columnar ice crystal growth regime. These LDR values were also consistent with scattering calculations for columnar ice crystals. Enhancements in LDR were suppressed within precipitation fallstreaks because the enhanced LDR values of columnar ice crystals were masked by the returns from the particles within the fallstreaks. However, Doppler velocity spectra of LDR within the fallstreak distinguished populations of slower-falling particles with high LDR (>−15 dB) and faster-falling particles with much lower LDR, suggesting that columnar ice crystals with high LDR coexisted with larger isometric particles that produced low LDR while dominating the total copolar reflectivity, thereby decreasing LDR. The measurements suggest that the columnar ice crystals originated in liquid-cloud layers through secondary ice production.

Corresponding author address: Mariko Oue, Dept. of Meteorology, The Pennsylvania State University, University Park, PA 16802. E-mail: muo15@psu.edu
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