Mathematical modeling of snow drifts transport by wind over the mountain terrain

In this paper, estimation of snow particles motion velocity and snow-drift density by mathematical modeling is studied. The snow particles flow is modeling from fluid dynamic concepts and micro-continuum approach (couple stresses fluid [1]). The present approach is compared to conventional classical...

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Main Author: Mahmoud Zarrini
Format: Article
Language:English
Published: University of Mohaghegh Ardabili 2013-12-01
Series:Journal of Hyperstructures
Subjects:
Online Access:https://jhs.uma.ac.ir/article_2567_c2b246248a13c874ca894d5dcb52140c.pdf
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author Mahmoud Zarrini
author_facet Mahmoud Zarrini
author_sort Mahmoud Zarrini
collection DOAJ
description In this paper, estimation of snow particles motion velocity and snow-drift density by mathematical modeling is studied. The snow particles flow is modeling from fluid dynamic concepts and micro-continuum approach (couple stresses fluid [1]). The present approach is compared to conventional classical approach of logarithmic law of snow-drift density ([2], [3]). It is shown that, the present approach yield better results than that of conventional approach.
format Article
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institution Matheson Library
issn 2251-8436
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language English
publishDate 2013-12-01
publisher University of Mohaghegh Ardabili
record_format Article
series Journal of Hyperstructures
spelling doaj-art-a9195d90ddca47b1b3d4c54ec2c5cb862025-07-09T08:23:30ZengUniversity of Mohaghegh ArdabiliJournal of Hyperstructures2251-84362322-16662013-12-012220120610.22098/jhs.2013.25672567Mathematical modeling of snow drifts transport by wind over the mountain terrainMahmoud Zarrini0Department of Applied Mathematics, University of Ayatollah Boroujerdi, Boroujerd, IranIn this paper, estimation of snow particles motion velocity and snow-drift density by mathematical modeling is studied. The snow particles flow is modeling from fluid dynamic concepts and micro-continuum approach (couple stresses fluid [1]). The present approach is compared to conventional classical approach of logarithmic law of snow-drift density ([2], [3]). It is shown that, the present approach yield better results than that of conventional approach.https://jhs.uma.ac.ir/article_2567_c2b246248a13c874ca894d5dcb52140c.pdfsnow particles velocitysnow drift densitycouple stress fluids
spellingShingle Mahmoud Zarrini
Mathematical modeling of snow drifts transport by wind over the mountain terrain
Journal of Hyperstructures
snow particles velocity
snow drift density
couple stress fluids
title Mathematical modeling of snow drifts transport by wind over the mountain terrain
title_full Mathematical modeling of snow drifts transport by wind over the mountain terrain
title_fullStr Mathematical modeling of snow drifts transport by wind over the mountain terrain
title_full_unstemmed Mathematical modeling of snow drifts transport by wind over the mountain terrain
title_short Mathematical modeling of snow drifts transport by wind over the mountain terrain
title_sort mathematical modeling of snow drifts transport by wind over the mountain terrain
topic snow particles velocity
snow drift density
couple stress fluids
url https://jhs.uma.ac.ir/article_2567_c2b246248a13c874ca894d5dcb52140c.pdf
work_keys_str_mv AT mahmoudzarrini mathematicalmodelingofsnowdriftstransportbywindoverthemountainterrain