This study presents the results from a series of wind-tunnel experiments designed to investigate the aerodynamic roughness length z0 of fresh snow under no-drift conditions. A two-component hot-film anemometer was employed to obtain vertical profiles of velocity statistics in a zero pressure gradient turbulent boundary layer for flow over naturally deposited snow surfaces. The roughness of these snow surfaces was measured by means of digital photography to capture characteristic length scales that can be related to z0. Our results show that, under aerodynamically rough conditions, the mean value of the roughness length for fresh snow is =0.24 mm with a standard deviation s(z0) = 0.05 mm. In this study, we show that variations in z0 are asso...
ABSTRACT. Spatial and temporal variations in aerodynamic roughness length (z0) on Haut Glacier d’Aro...
Calculation of the sensible and latent heat (turbulent) fluxes is required in order to close the sur...
A series of experiments have been made in a wind tunnel to investigate the ventilation of snow by sh...
This study presents the results from a series of wind-tunnel experiments designed to investigate the...
This study presents the results from a series of wind-tunnel experiments designed to investigate the...
This study presents the results from a series of wind-tunnel experiments designed to investigate the...
This study presents the results from a series of wind-tunnel experiments designed to investigate the...
We present results from a series of experiments in which fresh snow roughness was measured by means ...
Velocity profiles over fresh fallen snow surfaces have been measured in the SLF cold atmospheric bou...
When applied to a snow-covered surface, aerodynamic roughness length, z0, is typically considered as...
2022 Summer.Includes bibliographical references.Throughout the winter season, the snowpack becomes t...
Spatial and temporal variations in aerodynamic roughness length (z0) on Haut Glacier d'Arolla, Switz...
ABSTRACT. Spatial and temporal variations in aerodynamic roughness length (z0) on Haut Glacier d’Aro...
Calculation of the sensible and latent heat (turbulent) fluxes is required in order to close the sur...
A series of experiments have been made in a wind tunnel to investigate the ventilation of snow by sh...
This study presents the results from a series of wind-tunnel experiments designed to investigate the...
This study presents the results from a series of wind-tunnel experiments designed to investigate the...
This study presents the results from a series of wind-tunnel experiments designed to investigate the...
This study presents the results from a series of wind-tunnel experiments designed to investigate the...
We present results from a series of experiments in which fresh snow roughness was measured by means ...
Velocity profiles over fresh fallen snow surfaces have been measured in the SLF cold atmospheric bou...
When applied to a snow-covered surface, aerodynamic roughness length, z0, is typically considered as...
2022 Summer.Includes bibliographical references.Throughout the winter season, the snowpack becomes t...
Spatial and temporal variations in aerodynamic roughness length (z0) on Haut Glacier d'Arolla, Switz...
ABSTRACT. Spatial and temporal variations in aerodynamic roughness length (z0) on Haut Glacier d’Aro...
Calculation of the sensible and latent heat (turbulent) fluxes is required in order to close the sur...
A series of experiments have been made in a wind tunnel to investigate the ventilation of snow by sh...