A Review of Sintering in Seasonal Snow
WET SNOW
Slush
DRY SNOW
Rounded grains-continue
Figure 7. Snow grains stored at 24F for several years showing distinct grain-boundary grooves at the bonds
Figure 9. Equilibrium form of two grains of ice consisting of single crystals where the grain-boundary groove angle is 145
Figure 10. Two idealized particles shown at an early and the final stages of sintering
DISCUSSION AND CONCLUSIONS - CR97_100014
LITERATURE CITED - CR97_100015
LITERATURE CITED-continue - CR97_100016
Report Documentation Page - CR97_100017
CR97_10
WET SNOW
Slush
DRY SNOW
Rounded grains-continue
Figure 7. Snow grains stored at 24F for several years showing distinct grain-boundary grooves at the bonds
Figure 9. Equilibrium form of two grains of ice consisting of single crystals where the grain-boundary groove angle is 145
Figure 10. Two idealized particles shown at an early and the final stages of sintering
DISCUSSION AND CONCLUSIONS - CR97_100014
LITERATURE CITED - CR97_100015
LITERATURE CITED-continue - CR97_100016
Report Documentation Page - CR97_100017
CR97_10
