A Physically Based Model of the Form Drag Associated with Sastrugi
RAUPACH'S MODEL ADAPTED TO DRIFTED SNOW
Figure 3. Geometry of the sastrugi-like snowdrifts being modeled here
Partitioning the stress
Partitioning the stress-continue
Displacement height
RESULTS - CR95_160012
Figure 4. Model calculation of CDN10 as a function of the wind orientation (Φ) with respect to the dominant axis of the sastrugi
Figure 5. Stress partitioning, τR/τ, versus the mean wind direction with respect to the dominant axis of the sastrugi
DISCUSSION - CR95_160015
CONCLUSIONS - CR95_160016
LITERATURE CITED-continue - CR95_160017
Report Documentation Page - CR95_160018
CR95_16
RAUPACH'S MODEL ADAPTED TO DRIFTED SNOW
Figure 3. Geometry of the sastrugi-like snowdrifts being modeled here
Partitioning the stress
Partitioning the stress-continue
Displacement height
RESULTS - CR95_160012
Figure 4. Model calculation of CDN10 as a function of the wind orientation (Φ) with respect to the dominant axis of the sastrugi
Figure 5. Stress partitioning, τR/τ, versus the mean wind direction with respect to the dominant axis of the sastrugi
DISCUSSION - CR95_160015
CONCLUSIONS - CR95_160016
LITERATURE CITED-continue - CR95_160017
Report Documentation Page - CR95_160018
CR95_16