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A theoretical assessment of heat transfer by ventilation in homogeneous snowpacks

A theoretical assessment of heat transfer by ventilation in homogeneous snowpacks
A theoretical assessment of heat transfer by ventilation in homogeneous snowpacks
The effects of heat transfer by ventilation in snow are investigated theoretically. We draw together standard analytical results for fluid flow in porous media and apply them to the case of steady flows induced by periodic roughness elements. These solutions are used to estimate the relative magnitude of ventilation heat transfer in snow. We conclude that topography-driven ventilation is unlikely to have a significant impact on the larger scale energy balance of snow-covered regions since the airflow is confined to a shallow penetration depth or just the roughness elements themselves, rather than the bulk snowpack. In particular, for the limiting case of very warm and moisture saturated air flowing over a melting snow cover, we show that latent and sensible heat due to ventilation have about equal contributions and that this contribution is small compared to the overall surface flux as predicted by the Monin-Obukhov theory.
0043-1397
Bartlett, Stuart
d6942368-4dbc-4111-bce0-1867f4c60a89
Lehning, Michael
f5a19a3e-2785-4164-9e06-f97fcad140da
Bartlett, Stuart
d6942368-4dbc-4111-bce0-1867f4c60a89
Lehning, Michael
f5a19a3e-2785-4164-9e06-f97fcad140da

Bartlett, Stuart and Lehning, Michael (2011) A theoretical assessment of heat transfer by ventilation in homogeneous snowpacks. Water Resources Research, 47.

Record type: Article

Abstract

The effects of heat transfer by ventilation in snow are investigated theoretically. We draw together standard analytical results for fluid flow in porous media and apply them to the case of steady flows induced by periodic roughness elements. These solutions are used to estimate the relative magnitude of ventilation heat transfer in snow. We conclude that topography-driven ventilation is unlikely to have a significant impact on the larger scale energy balance of snow-covered regions since the airflow is confined to a shallow penetration depth or just the roughness elements themselves, rather than the bulk snowpack. In particular, for the limiting case of very warm and moisture saturated air flowing over a melting snow cover, we show that latent and sensible heat due to ventilation have about equal contributions and that this contribution is small compared to the overall surface flux as predicted by the Monin-Obukhov theory.

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More information

Published date: 7 April 2011
Organisations: Agents, Interactions & Complexity

Identifiers

Local EPrints ID: 272160
URI: http://eprints.soton.ac.uk/id/eprint/272160
ISSN: 0043-1397
PURE UUID: 4845bfcd-24b0-4098-845f-31397c33d04e

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Date deposited: 07 Apr 2011 09:34
Last modified: 16 Jul 2019 22:15

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Contributors

Author: Stuart Bartlett
Author: Michael Lehning

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