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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Format: | Article |
Language: | English |
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University of Mohaghegh Ardabili
2013-12-01
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Series: | Journal of Hyperstructures |
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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 |
id | doaj-art-a9195d90ddca47b1b3d4c54ec2c5cb86 |
institution | Matheson Library |
issn | 2251-8436 2322-1666 |
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 |