Differential radar scattering properties of model hail and mixed‐phase hydrometeors

Kultegin Aydin, T. A. Seliga, V. N. Bringi

Research output: Contribution to journalArticle

35 Citations (Scopus)

Abstract

The differential reflectivity (ZDR) radar signal contains information on the shape and alignment of ice phase hydrometeors. Under certain circumstances, then, this signal and reflectivity factor can be used to identify the presence of hail particles. Such interpretations require knowledge about the scattering properties of various types and shapes of hydrometeors, including ice, water‐coated ice, and graupel. These hydrometeors are examined for their differential scattering properties obtained from computations using the transition (T) matrix method of Waterman and an extension of this theory to two‐layered bodies. Differential radar cross sections together with circular depolarization ratios are presented, and several instances of possible hail detection by radar using ZDR signatures are illustrated.

Original languageEnglish (US)
Pages (from-to)58-66
Number of pages9
JournalRadio Science
Volume19
Issue number1
DOIs
StatePublished - Jan 1 1984

Fingerprint

hail
radar scattering
hydrometeors
Precipitation (meteorology)
Ice
ice
Radar
scattering
radar
Scattering
reflectivity
graupel
reflectance
radar cross sections
Radar cross section
Depolarization
depolarization
matrix methods
cross section
alignment

All Science Journal Classification (ASJC) codes

  • Condensed Matter Physics
  • Earth and Planetary Sciences(all)
  • Electrical and Electronic Engineering

Cite this

Aydin, Kultegin ; Seliga, T. A. ; Bringi, V. N. / Differential radar scattering properties of model hail and mixed‐phase hydrometeors. In: Radio Science. 1984 ; Vol. 19, No. 1. pp. 58-66.
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Differential radar scattering properties of model hail and mixed‐phase hydrometeors. / Aydin, Kultegin; Seliga, T. A.; Bringi, V. N.

In: Radio Science, Vol. 19, No. 1, 01.01.1984, p. 58-66.

Research output: Contribution to journalArticle

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