Parameterization of single-scattering properties of snow

Snow consists of non-spherical grains of various shapes and sizes. Still, in many radiative transfer applications, single-scattering properties of snow have been based on the assumption of spherical grains. More recently, second-generation Koch fractals have been employed. While they produce a relat...

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Published in:The Cryosphere
Main Authors: Räisänen, P., Kokhanovsky, A., Guyot, G., Jourdan, O., Nousiainen, T.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-9-1277-2015
https://tc.copernicus.org/articles/9/1277/2015/
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spelling ftcopernicus:oai:publications.copernicus.org:tc28345 2023-05-15T17:48:28+02:00 Parameterization of single-scattering properties of snow Räisänen, P. Kokhanovsky, A. Guyot, G. Jourdan, O. Nousiainen, T. 2018-09-27 application/pdf https://doi.org/10.5194/tc-9-1277-2015 https://tc.copernicus.org/articles/9/1277/2015/ eng eng doi:10.5194/tc-9-1277-2015 https://tc.copernicus.org/articles/9/1277/2015/ eISSN: 1994-0424 Text 2018 ftcopernicus https://doi.org/10.5194/tc-9-1277-2015 2020-07-20T16:24:33Z Snow consists of non-spherical grains of various shapes and sizes. Still, in many radiative transfer applications, single-scattering properties of snow have been based on the assumption of spherical grains. More recently, second-generation Koch fractals have been employed. While they produce a relatively flat phase function typical of deformed non-spherical particles, this is still a rather ad hoc choice. Here, angular scattering measurements for blowing snow conducted during the CLimate IMpacts of Short-Lived pollutants In the Polar region (CLIMSLIP) campaign at Ny Ålesund, Svalbard, are used to construct a reference phase function for snow. Based on this phase function, an optimized habit combination (OHC) consisting of severely rough (SR) droxtals, aggregates of SR plates and strongly distorted Koch fractals is selected. The single-scattering properties of snow are then computed for the OHC as a function of wavelength λ and snow grain volume-to-projected area equivalent radius r vp . Parameterization equations are developed for λ = 0.199–2.7 μm and r vp = 10–2000 μm, which express the single-scattering co-albedo β, the asymmetry parameter g and the phase function P 11 as functions of the size parameter and the real and imaginary parts of the refractive index. The parameterizations are analytic and simple to use in radiative transfer models. Compared to the reference values computed for the OHC, the accuracy of the parameterization is very high for β and g . This is also true for the phase function parameterization, except for strongly absorbing cases (β > 0.3). Finally, we consider snow albedo and reflected radiances for the suggested snow optics parameterization, making comparisons to spheres and distorted Koch fractals. Text Ny Ålesund Ny-Ålesund Svalbard Copernicus Publications: E-Journals Ny-Ålesund Svalbard The Cryosphere 9 3 1277 1301
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Snow consists of non-spherical grains of various shapes and sizes. Still, in many radiative transfer applications, single-scattering properties of snow have been based on the assumption of spherical grains. More recently, second-generation Koch fractals have been employed. While they produce a relatively flat phase function typical of deformed non-spherical particles, this is still a rather ad hoc choice. Here, angular scattering measurements for blowing snow conducted during the CLimate IMpacts of Short-Lived pollutants In the Polar region (CLIMSLIP) campaign at Ny Ålesund, Svalbard, are used to construct a reference phase function for snow. Based on this phase function, an optimized habit combination (OHC) consisting of severely rough (SR) droxtals, aggregates of SR plates and strongly distorted Koch fractals is selected. The single-scattering properties of snow are then computed for the OHC as a function of wavelength λ and snow grain volume-to-projected area equivalent radius r vp . Parameterization equations are developed for λ = 0.199–2.7 μm and r vp = 10–2000 μm, which express the single-scattering co-albedo β, the asymmetry parameter g and the phase function P 11 as functions of the size parameter and the real and imaginary parts of the refractive index. The parameterizations are analytic and simple to use in radiative transfer models. Compared to the reference values computed for the OHC, the accuracy of the parameterization is very high for β and g . This is also true for the phase function parameterization, except for strongly absorbing cases (β > 0.3). Finally, we consider snow albedo and reflected radiances for the suggested snow optics parameterization, making comparisons to spheres and distorted Koch fractals.
format Text
author Räisänen, P.
Kokhanovsky, A.
Guyot, G.
Jourdan, O.
Nousiainen, T.
spellingShingle Räisänen, P.
Kokhanovsky, A.
Guyot, G.
Jourdan, O.
Nousiainen, T.
Parameterization of single-scattering properties of snow
author_facet Räisänen, P.
Kokhanovsky, A.
Guyot, G.
Jourdan, O.
Nousiainen, T.
author_sort Räisänen, P.
title Parameterization of single-scattering properties of snow
title_short Parameterization of single-scattering properties of snow
title_full Parameterization of single-scattering properties of snow
title_fullStr Parameterization of single-scattering properties of snow
title_full_unstemmed Parameterization of single-scattering properties of snow
title_sort parameterization of single-scattering properties of snow
publishDate 2018
url https://doi.org/10.5194/tc-9-1277-2015
https://tc.copernicus.org/articles/9/1277/2015/
geographic Ny-Ålesund
Svalbard
geographic_facet Ny-Ålesund
Svalbard
genre Ny Ålesund
Ny-Ålesund
Svalbard
genre_facet Ny Ålesund
Ny-Ålesund
Svalbard
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-9-1277-2015
https://tc.copernicus.org/articles/9/1277/2015/
op_doi https://doi.org/10.5194/tc-9-1277-2015
container_title The Cryosphere
container_volume 9
container_issue 3
container_start_page 1277
op_container_end_page 1301
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