### Abstract

The equations of motion (continuity and momentum balance) for a dispersed, negatively buoyant particulate of snow entrained in a turbulent airflow contain apparent turbulent forces or turbulent particle buoyancies. These turbulent buoyancies arise from the constitutive assumption that the turbulent fluctuations of the snow phase velocity vector, and the drift snow density are proportional to the deviatoric mean rate of deformation tensor for the airflow. For an established, discretized airflow regime, the momentum balance equation for the snow phase can be solved by finite difference techniques for the snow particle velocity field. The snow phase continuity equation can then be solved for the drift snow density field. (from authors' abstract)

Original language | English (US) |
---|---|

Title of host publication | IN: ANNALS OF GLACIOLOGY, PROC. SYMP. ON SNOW AND ICE PROCESSES AT THE EARTH'S SURFACE, (SAPPORO, JAPAN: SEP. 2-7, 1984) |

Publisher | Int. Glaciol. Soc |

Volume | 6 , Cambridge, U.K., Int. Glaciol. Soc., 1985, p.53-58. |

ISBN (Print) | 0 9502484 79 |

State | Published - 1985 |

Externally published | Yes |

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### ASJC Scopus subject areas

- Earth and Planetary Sciences (miscellaneous)

### Cite this

*IN: ANNALS OF GLACIOLOGY, PROC. SYMP. ON SNOW AND ICE PROCESSES AT THE EARTH'S SURFACE, (SAPPORO, JAPAN: SEP. 2-7, 1984)*(Vol. 6 , Cambridge, U.K., Int. Glaciol. Soc., 1985, p.53-58.). Int. Glaciol. Soc.

**Two dimensional solutions for a turbulent continuum theory for the atmospheric mixture of snow and air.** / Decker, Rand; Brown, R. L.

Research output: Chapter in Book/Report/Conference proceeding › Chapter

*IN: ANNALS OF GLACIOLOGY, PROC. SYMP. ON SNOW AND ICE PROCESSES AT THE EARTH'S SURFACE, (SAPPORO, JAPAN: SEP. 2-7, 1984).*vol. 6 , Cambridge, U.K., Int. Glaciol. Soc., 1985, p.53-58., Int. Glaciol. Soc.

}

TY - CHAP

T1 - Two dimensional solutions for a turbulent continuum theory for the atmospheric mixture of snow and air.

AU - Decker, Rand

AU - Brown, R. L.

PY - 1985

Y1 - 1985

N2 - The equations of motion (continuity and momentum balance) for a dispersed, negatively buoyant particulate of snow entrained in a turbulent airflow contain apparent turbulent forces or turbulent particle buoyancies. These turbulent buoyancies arise from the constitutive assumption that the turbulent fluctuations of the snow phase velocity vector, and the drift snow density are proportional to the deviatoric mean rate of deformation tensor for the airflow. For an established, discretized airflow regime, the momentum balance equation for the snow phase can be solved by finite difference techniques for the snow particle velocity field. The snow phase continuity equation can then be solved for the drift snow density field. (from authors' abstract)

AB - The equations of motion (continuity and momentum balance) for a dispersed, negatively buoyant particulate of snow entrained in a turbulent airflow contain apparent turbulent forces or turbulent particle buoyancies. These turbulent buoyancies arise from the constitutive assumption that the turbulent fluctuations of the snow phase velocity vector, and the drift snow density are proportional to the deviatoric mean rate of deformation tensor for the airflow. For an established, discretized airflow regime, the momentum balance equation for the snow phase can be solved by finite difference techniques for the snow particle velocity field. The snow phase continuity equation can then be solved for the drift snow density field. (from authors' abstract)

UR - http://www.scopus.com/inward/record.url?scp=17444435159&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=17444435159&partnerID=8YFLogxK

M3 - Chapter

SN - 0 9502484 79

VL - 6 , Cambridge, U.K., Int. Glaciol. Soc., 1985, p.53-58.

BT - IN: ANNALS OF GLACIOLOGY, PROC. SYMP. ON SNOW AND ICE PROCESSES AT THE EARTH'S SURFACE, (SAPPORO, JAPAN: SEP. 2-7, 1984)

PB - Int. Glaciol. Soc

ER -