Input for a blowing snow numerical model: in situ measurements are still needed
The NEMO numerical model of drifting snow, whose general outlines are presented in this paper, is based on a physical model for saltation and turbulent diffusion. The model needs a set of input parameters including fall velocity, threshold shear velocity, shear velocity, mass concentration and rough...
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ftcemoa:oai:irsteadoc.irstea.fr:PUB00026035 2023-05-15T13:54:06+02:00 Input for a blowing snow numerical model: in situ measurements are still needed Naaim Bouvet, F. Bellot, H. Cierco, F.X. Naaïm, M. CEMAGREF GRENOBLE ETGR 2008 application/pdf https://irsteadoc.irstea.fr/cemoa/PUB00026035 Anglais eng https://irsteadoc.irstea.fr/cemoa/PUB00026035 Date de dépôt: 2009-02-24 - Tous les documents et informations contenus dans la base CemOA Publications sont protégés en vertu du droit de propriété intellectuelle, en particulier par le droit d'auteur. La personne consultant la base CemOA Publications peut visualiser, reproduire, ou stocker des copies des publications, à condition que l'information soit seulement pour son usage personnel et non commercial. L'utilisation des travaux universitaires est soumise à autorisation préalable de leurs auteurs. Toute information relative au signalement d'une publication contenue dans CemOA Publications doit inclure la citation bibliographique usuelle : Nom du ou des auteurs, titre et source du document, date et URL de la notice (dc_identifier). 21659 TRANSPORT DE NEIGE PAR LE VENT MODELE NUMERIQUE MESURE MEASUREMENT DRIFTING SNOW NUMERICAL MODEL Communication scientifique avec actes 2008 ftcemoa 2021-06-29T09:15:15Z The NEMO numerical model of drifting snow, whose general outlines are presented in this paper, is based on a physical model for saltation and turbulent diffusion. The model needs a set of input parameters including fall velocity, threshold shear velocity, shear velocity, mass concentration and roughness, which are obtained from empirical formulae and wind speed measured at a given height. To better determine the required field data in an alpine context, our experimental site, Col du Lac Blanc (2700 m) in the French Alps, was first equipped with blowing snow acoustic sensors, which proved not to be accurate enough for research purposes in the current state of development even though a new calibration curve was used. We therefore returned to the traditional, robust mechanical traps and a 10-m mast with six anemometers, two temperature sensors and a depth sensor to better determine friction velocity and aerodynamic roughness. For the drifting snow events studied, (i) the proportionality of the aerodynamic roughness to the square of the friction velocity was confirmed but with a proportionality ratio depending on the snow drift event, (ii) values or σs UF were relatively well approximated by empirical formulae obtained from Antarctica data, and (iii) snowdrift concentration profiles obtained by Pomeroy's semi-empirical formulae for saltation layer coupled with theoretical approach for the diffusion layer overestimated the concentration profiles for the studied blowing snow event. Other/Unknown Material Antarc* Antarctica Irstea Publications et Bases documentaires (Irstea@doc/CemOA) Lac Blanc ENVELOPE(68.917,68.917,-49.217,-49.217) |
institution |
Open Polar |
collection |
Irstea Publications et Bases documentaires (Irstea@doc/CemOA) |
op_collection_id |
ftcemoa |
language |
English |
topic |
TRANSPORT DE NEIGE PAR LE VENT MODELE NUMERIQUE MESURE MEASUREMENT DRIFTING SNOW NUMERICAL MODEL |
spellingShingle |
TRANSPORT DE NEIGE PAR LE VENT MODELE NUMERIQUE MESURE MEASUREMENT DRIFTING SNOW NUMERICAL MODEL Naaim Bouvet, F. Bellot, H. Cierco, F.X. Naaïm, M. Input for a blowing snow numerical model: in situ measurements are still needed |
topic_facet |
TRANSPORT DE NEIGE PAR LE VENT MODELE NUMERIQUE MESURE MEASUREMENT DRIFTING SNOW NUMERICAL MODEL |
description |
The NEMO numerical model of drifting snow, whose general outlines are presented in this paper, is based on a physical model for saltation and turbulent diffusion. The model needs a set of input parameters including fall velocity, threshold shear velocity, shear velocity, mass concentration and roughness, which are obtained from empirical formulae and wind speed measured at a given height. To better determine the required field data in an alpine context, our experimental site, Col du Lac Blanc (2700 m) in the French Alps, was first equipped with blowing snow acoustic sensors, which proved not to be accurate enough for research purposes in the current state of development even though a new calibration curve was used. We therefore returned to the traditional, robust mechanical traps and a 10-m mast with six anemometers, two temperature sensors and a depth sensor to better determine friction velocity and aerodynamic roughness. For the drifting snow events studied, (i) the proportionality of the aerodynamic roughness to the square of the friction velocity was confirmed but with a proportionality ratio depending on the snow drift event, (ii) values or σs UF were relatively well approximated by empirical formulae obtained from Antarctica data, and (iii) snowdrift concentration profiles obtained by Pomeroy's semi-empirical formulae for saltation layer coupled with theoretical approach for the diffusion layer overestimated the concentration profiles for the studied blowing snow event. |
author2 |
CEMAGREF GRENOBLE ETGR |
format |
Other/Unknown Material |
author |
Naaim Bouvet, F. Bellot, H. Cierco, F.X. Naaïm, M. |
author_facet |
Naaim Bouvet, F. Bellot, H. Cierco, F.X. Naaïm, M. |
author_sort |
Naaim Bouvet, F. |
title |
Input for a blowing snow numerical model: in situ measurements are still needed |
title_short |
Input for a blowing snow numerical model: in situ measurements are still needed |
title_full |
Input for a blowing snow numerical model: in situ measurements are still needed |
title_fullStr |
Input for a blowing snow numerical model: in situ measurements are still needed |
title_full_unstemmed |
Input for a blowing snow numerical model: in situ measurements are still needed |
title_sort |
input for a blowing snow numerical model: in situ measurements are still needed |
publishDate |
2008 |
url |
https://irsteadoc.irstea.fr/cemoa/PUB00026035 |
long_lat |
ENVELOPE(68.917,68.917,-49.217,-49.217) |
geographic |
Lac Blanc |
geographic_facet |
Lac Blanc |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
21659 |
op_relation |
https://irsteadoc.irstea.fr/cemoa/PUB00026035 |
op_rights |
Date de dépôt: 2009-02-24 - Tous les documents et informations contenus dans la base CemOA Publications sont protégés en vertu du droit de propriété intellectuelle, en particulier par le droit d'auteur. La personne consultant la base CemOA Publications peut visualiser, reproduire, ou stocker des copies des publications, à condition que l'information soit seulement pour son usage personnel et non commercial. L'utilisation des travaux universitaires est soumise à autorisation préalable de leurs auteurs. Toute information relative au signalement d'une publication contenue dans CemOA Publications doit inclure la citation bibliographique usuelle : Nom du ou des auteurs, titre et source du document, date et URL de la notice (dc_identifier). |
_version_ |
1766259759314370560 |