Application Of Micro-Continuum Approach In The Estimation Of Snow Drift Density, Velocity And Mass Transport In Hilly Bound Cold Regions

We estimate snow velocity and snow drift density on hilly terrain under the assumption that the drifting snow mass can be represented using a micro-continuum approach (i.e. using a nonclassical mechanics approach assuming a class of fluids for which basic equations of mass, momentum and energy have...

Full description

Bibliographic Details
Main Authors: Zarrini, Mahmoud, R. N. Pralhad
Format: Text
Language:English
Published: Zenodo 2011
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.1060417
https://zenodo.org/record/1060417
id ftdatacite:10.5281/zenodo.1060417
record_format openpolar
spelling ftdatacite:10.5281/zenodo.1060417 2023-05-15T14:04:42+02:00 Application Of Micro-Continuum Approach In The Estimation Of Snow Drift Density, Velocity And Mass Transport In Hilly Bound Cold Regions Zarrini, Mahmoud R. N. Pralhad 2011 https://dx.doi.org/10.5281/zenodo.1060417 https://zenodo.org/record/1060417 en eng Zenodo https://dx.doi.org/10.5281/zenodo.1060416 Open Access Creative Commons Attribution 4.0 https://creativecommons.org/licenses/by/4.0 info:eu-repo/semantics/openAccess CC-BY Snow velocity snow drift density mass transport of snow particles snow avalanche. Text Journal article article-journal ScholarlyArticle 2011 ftdatacite https://doi.org/10.5281/zenodo.1060417 https://doi.org/10.5281/zenodo.1060416 2021-11-05T12:55:41Z We estimate snow velocity and snow drift density on hilly terrain under the assumption that the drifting snow mass can be represented using a micro-continuum approach (i.e. using a nonclassical mechanics approach assuming a class of fluids for which basic equations of mass, momentum and energy have been derived). In our model, the theory of coupled stress fluids proposed by Stokes [1] has been employed for the computation of flow parameters. Analyses of bulk drift velocity, drift density, drift transport and mass transport of snow particles have been carried out and computations made, considering various parametric effects. Results are compared with those of classical mechanics (logarithmic wind profile). The results indicate that particle size affects the flow characteristics significantly. : {"references": ["V.K. Stokes, Couple stresses in Fluids. Phys Fluids 9, 1710-15, 1966.", "R.A. Bagnold, The physics of blown sand and desert dunes. William\nmorrow and company, 1941.", "W. Budd, R. Dingle and W. Radok, Byrd snow drift project . , 1966.", "R. Kawamura, Study on sand moment by wind. , 1951.", "G.H. Liljequist, Energy Exchange of an Antarctic Snowfield, Wind Structure\nin the Low Layer, \"Norwegian-British-Swedish Antarctic Expedition,\n1949-52\". scientific Results, Vol. 2, part 1C, 187-233, 1957.", "M. Mellor, Blowing snow U.S. Cold Regions Research and Engineering\nLaboratory. Cold regions science and Engineering Hanover, N.H., pt.\nIII, section A3c, 1965.", "M. Mellor, A drift review of snow drifts research. Technical Report\nCRSE III-A3d, Cold Regions Research Engineering Laboratory, 1974.", "R.A. Schmidt, Wind Flow over Alpine ridges, Ph.D. dissertation. (USA),\n1967.", "Paul M.B. Fohn, Snow Transport over mountain crests. Journal of\nGlaciology vol. 26, No. 94, 1980.\n[10] D. Kobayashi, Studies of Snow transport in low level drifting snow.\ncontributions from the Institute of low temperature science, series A, No.\n24, 1971.\n[11] Y.C. Fung, A First course in continuum mechanics. Prentice Hall, 1993.\n[12] S.C. Cowin, The theory of polar fluids. Adv. In Appl. Mech. 14, 279-\n347, 1974.\n[13] A.C. Eringan, Theory of micro polar fluids. J. Math. Mech. 16, 1-18,\n1966.\n[14] F.M. White, Fluid Mechanics. Mc-Graw-Hill, 2003.\n[15] D.M. McClung, Derivation of Voellmy-s maximum speed and run-out\nestimates from a centre of mass model. Journal of Glaciology, 29(102),\n1983."]} Text Antarc* Antarctic DataCite Metadata Store (German National Library of Science and Technology) Antarctic Bagnold ENVELOPE(-67.483,-67.483,-67.033,-67.033) Byrd Dingle ENVELOPE(78.066,78.066,-68.567,-68.567) McClung ENVELOPE(-144.433,-144.433,-77.183,-77.183) Mellor ENVELOPE(-114.944,-114.944,60.714,60.714)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Snow velocity
snow drift density
mass transport of snow particles
snow avalanche.
spellingShingle Snow velocity
snow drift density
mass transport of snow particles
snow avalanche.
Zarrini, Mahmoud
R. N. Pralhad
Application Of Micro-Continuum Approach In The Estimation Of Snow Drift Density, Velocity And Mass Transport In Hilly Bound Cold Regions
topic_facet Snow velocity
snow drift density
mass transport of snow particles
snow avalanche.
description We estimate snow velocity and snow drift density on hilly terrain under the assumption that the drifting snow mass can be represented using a micro-continuum approach (i.e. using a nonclassical mechanics approach assuming a class of fluids for which basic equations of mass, momentum and energy have been derived). In our model, the theory of coupled stress fluids proposed by Stokes [1] has been employed for the computation of flow parameters. Analyses of bulk drift velocity, drift density, drift transport and mass transport of snow particles have been carried out and computations made, considering various parametric effects. Results are compared with those of classical mechanics (logarithmic wind profile). The results indicate that particle size affects the flow characteristics significantly. : {"references": ["V.K. Stokes, Couple stresses in Fluids. Phys Fluids 9, 1710-15, 1966.", "R.A. Bagnold, The physics of blown sand and desert dunes. William\nmorrow and company, 1941.", "W. Budd, R. Dingle and W. Radok, Byrd snow drift project . , 1966.", "R. Kawamura, Study on sand moment by wind. , 1951.", "G.H. Liljequist, Energy Exchange of an Antarctic Snowfield, Wind Structure\nin the Low Layer, \"Norwegian-British-Swedish Antarctic Expedition,\n1949-52\". scientific Results, Vol. 2, part 1C, 187-233, 1957.", "M. Mellor, Blowing snow U.S. Cold Regions Research and Engineering\nLaboratory. Cold regions science and Engineering Hanover, N.H., pt.\nIII, section A3c, 1965.", "M. Mellor, A drift review of snow drifts research. Technical Report\nCRSE III-A3d, Cold Regions Research Engineering Laboratory, 1974.", "R.A. Schmidt, Wind Flow over Alpine ridges, Ph.D. dissertation. (USA),\n1967.", "Paul M.B. Fohn, Snow Transport over mountain crests. Journal of\nGlaciology vol. 26, No. 94, 1980.\n[10] D. Kobayashi, Studies of Snow transport in low level drifting snow.\ncontributions from the Institute of low temperature science, series A, No.\n24, 1971.\n[11] Y.C. Fung, A First course in continuum mechanics. Prentice Hall, 1993.\n[12] S.C. Cowin, The theory of polar fluids. Adv. In Appl. Mech. 14, 279-\n347, 1974.\n[13] A.C. Eringan, Theory of micro polar fluids. J. Math. Mech. 16, 1-18,\n1966.\n[14] F.M. White, Fluid Mechanics. Mc-Graw-Hill, 2003.\n[15] D.M. McClung, Derivation of Voellmy-s maximum speed and run-out\nestimates from a centre of mass model. Journal of Glaciology, 29(102),\n1983."]}
format Text
author Zarrini, Mahmoud
R. N. Pralhad
author_facet Zarrini, Mahmoud
R. N. Pralhad
author_sort Zarrini, Mahmoud
title Application Of Micro-Continuum Approach In The Estimation Of Snow Drift Density, Velocity And Mass Transport In Hilly Bound Cold Regions
title_short Application Of Micro-Continuum Approach In The Estimation Of Snow Drift Density, Velocity And Mass Transport In Hilly Bound Cold Regions
title_full Application Of Micro-Continuum Approach In The Estimation Of Snow Drift Density, Velocity And Mass Transport In Hilly Bound Cold Regions
title_fullStr Application Of Micro-Continuum Approach In The Estimation Of Snow Drift Density, Velocity And Mass Transport In Hilly Bound Cold Regions
title_full_unstemmed Application Of Micro-Continuum Approach In The Estimation Of Snow Drift Density, Velocity And Mass Transport In Hilly Bound Cold Regions
title_sort application of micro-continuum approach in the estimation of snow drift density, velocity and mass transport in hilly bound cold regions
publisher Zenodo
publishDate 2011
url https://dx.doi.org/10.5281/zenodo.1060417
https://zenodo.org/record/1060417
long_lat ENVELOPE(-67.483,-67.483,-67.033,-67.033)
ENVELOPE(78.066,78.066,-68.567,-68.567)
ENVELOPE(-144.433,-144.433,-77.183,-77.183)
ENVELOPE(-114.944,-114.944,60.714,60.714)
geographic Antarctic
Bagnold
Byrd
Dingle
McClung
Mellor
geographic_facet Antarctic
Bagnold
Byrd
Dingle
McClung
Mellor
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation https://dx.doi.org/10.5281/zenodo.1060416
op_rights Open Access
Creative Commons Attribution 4.0
https://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5281/zenodo.1060417
https://doi.org/10.5281/zenodo.1060416
_version_ 1766275931336343552