2001
DOI: 10.1364/ao.40.003092
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Radar and scattering parameters through falling hydrometeors with axisymmetric shapes

Abstract: Falling raindrops and other hydrometeors have, in general, nonspherical shapes and mean canting angles that are due to aerodynamic and gravitational forces. We use the T matrix and the quantum theory of angular momentum to compute extinction matrices, scattering and absorption cross sections, backscattering matrices, and, from these quantities, radar parameters. A monodisperse population of rain with axially symmetric distribution over orientations where the axis of symmetry is the local direction of air flow … Show more

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Cited by 7 publications
(3 citation statements)
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References 13 publications
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“…Pludix is a rain gauge disdrometer that analyses the signal backscattered by hydrometeors [ Prodi et al , 2000; Battaglia et al , 2001]. It is an upward‐looking, bi‐static system (i.e.…”
Section: Measurement Of the Terminal Settling Velocity Of Volcanic Pamentioning
confidence: 99%
“…Pludix is a rain gauge disdrometer that analyses the signal backscattered by hydrometeors [ Prodi et al , 2000; Battaglia et al , 2001]. It is an upward‐looking, bi‐static system (i.e.…”
Section: Measurement Of the Terminal Settling Velocity Of Volcanic Pamentioning
confidence: 99%
“…During the last two decades, weather-dedicated radar and optical disdrometers have been introduced in volcanology to determine the size and velocity of tephra falling at various volcanoes such as Etna 5 , Eyjafjallajökull 6 , Sakurajima 7 11 and Stromboli 12 14 . The optical disdrometers have the advantage of determining size and velocity simultaneously, allowing for a better characterization of tephra particles, whereas radar disdrometers require additional backscatter models to provide particle sizes 5 , 6 , 15 . These optical instruments have been tested under various field conditions and represent one of the most promising techniques to determine GSDs and ground accumulation in real time, based on direct measurements of settling particles.…”
Section: Introductionmentioning
confidence: 99%
“…There are two linear relation nominations, line A, with equation "a/b = 1−0.1a o " and line B, with (a/b = 1 − (0.41/4.5)a o ) which are used for axial ratio calculations. In these equations, a o is equal to the raindrop mean radius in millimeters and a nonlinear equation for axial ration is assumed as [6]:…”
Section: Introductionmentioning
confidence: 99%