Microwave single-scattering properties of randomly oriented soft-ice hydrometeors

Large ice hydrometeors are usually present in intense convective clouds and may significantly affect the upwelling radiances that are measured by satellite-borne microwave radiometers – especially, at millimeter-wavelength frequencies. Thus, interpretation of these measurements (e.g., for precipitat...

Full description

Bibliographic Details
Main Authors: D. Casella, A. Mugnai, P. Sanò, M. Formenton
Format: Article
Language:English
Published: Copernicus Publications 2008-11-01
Series:Advances in Geosciences
Online Access:http://www.adv-geosci.net/17/79/2008/adgeo-17-79-2008.pdf
id doaj-19333985ce2f48b88f9c8bea00c8e21e
record_format Article
spelling doaj-19333985ce2f48b88f9c8bea00c8e21e2020-11-25T01:35:10ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592008-11-01177985Microwave single-scattering properties of randomly oriented soft-ice hydrometeorsD. CasellaA. MugnaiP. SanòM. FormentonLarge ice hydrometeors are usually present in intense convective clouds and may significantly affect the upwelling radiances that are measured by satellite-borne microwave radiometers – especially, at millimeter-wavelength frequencies. Thus, interpretation of these measurements (e.g., for precipitation retrieval) requires knowledge of the single scattering properties of ice particles. On the other hand, shape and internal structure of these particles (especially, the larger ones) is very complex and variable, and therefore it is necessary to resort to simplifying assumptions in order to compute their single-scattering parameters. <br><br> In this study, we use the discrete dipole approximation (DDA) to compute the absorption and scattering efficiencies and the asymmetry factor of two kinds of quasi-spherical and non-homogeneous soft-ice particles in the frequency range 50–183 GHz. Particles of the first kind are modeled as quasi-spherical ice particles having randomly distributed spherical air inclusions. Particles of the second kind are modeled as random aggregates of ice spheres having random radii. In both cases, particle densities and dimensions are coherent with the snow hydrometeor category that is utilized by the University of Wisconsin – Non-hydrostatic Modeling System (UW-NMS) cloud-mesoscale model. Then, we compare our single-scattering results for randomly-oriented soft-ice hydrometeors with corresponding ones that make use of: a) effective-medium equivalent spheres, b) solid-ice equivalent spheres, and c) randomly-oriented aggregates of ice cylinders. Finally, we extend to our particles the scattering formulas that have been developed by other authors for randomly-oriented aggregates of ice cylinders. http://www.adv-geosci.net/17/79/2008/adgeo-17-79-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. Casella
A. Mugnai
P. Sanò
M. Formenton
spellingShingle D. Casella
A. Mugnai
P. Sanò
M. Formenton
Microwave single-scattering properties of randomly oriented soft-ice hydrometeors
Advances in Geosciences
author_facet D. Casella
A. Mugnai
P. Sanò
M. Formenton
author_sort D. Casella
title Microwave single-scattering properties of randomly oriented soft-ice hydrometeors
title_short Microwave single-scattering properties of randomly oriented soft-ice hydrometeors
title_full Microwave single-scattering properties of randomly oriented soft-ice hydrometeors
title_fullStr Microwave single-scattering properties of randomly oriented soft-ice hydrometeors
title_full_unstemmed Microwave single-scattering properties of randomly oriented soft-ice hydrometeors
title_sort microwave single-scattering properties of randomly oriented soft-ice hydrometeors
publisher Copernicus Publications
series Advances in Geosciences
issn 1680-7340
1680-7359
publishDate 2008-11-01
description Large ice hydrometeors are usually present in intense convective clouds and may significantly affect the upwelling radiances that are measured by satellite-borne microwave radiometers – especially, at millimeter-wavelength frequencies. Thus, interpretation of these measurements (e.g., for precipitation retrieval) requires knowledge of the single scattering properties of ice particles. On the other hand, shape and internal structure of these particles (especially, the larger ones) is very complex and variable, and therefore it is necessary to resort to simplifying assumptions in order to compute their single-scattering parameters. <br><br> In this study, we use the discrete dipole approximation (DDA) to compute the absorption and scattering efficiencies and the asymmetry factor of two kinds of quasi-spherical and non-homogeneous soft-ice particles in the frequency range 50–183 GHz. Particles of the first kind are modeled as quasi-spherical ice particles having randomly distributed spherical air inclusions. Particles of the second kind are modeled as random aggregates of ice spheres having random radii. In both cases, particle densities and dimensions are coherent with the snow hydrometeor category that is utilized by the University of Wisconsin – Non-hydrostatic Modeling System (UW-NMS) cloud-mesoscale model. Then, we compare our single-scattering results for randomly-oriented soft-ice hydrometeors with corresponding ones that make use of: a) effective-medium equivalent spheres, b) solid-ice equivalent spheres, and c) randomly-oriented aggregates of ice cylinders. Finally, we extend to our particles the scattering formulas that have been developed by other authors for randomly-oriented aggregates of ice cylinders.
url http://www.adv-geosci.net/17/79/2008/adgeo-17-79-2008.pdf
work_keys_str_mv AT dcasella microwavesinglescatteringpropertiesofrandomlyorientedsofticehydrometeors
AT amugnai microwavesinglescatteringpropertiesofrandomlyorientedsofticehydrometeors
AT psano microwavesinglescatteringpropertiesofrandomlyorientedsofticehydrometeors
AT mformenton microwavesinglescatteringpropertiesofrandomlyorientedsofticehydrometeors
_version_ 1725068067358113792