Parameterizing Scalar Transfer over Snow and Ice: A Review

Parameterizing Scalar Transfer over Snow and Ice: A Review AbstractEvaluating the profiles of wind speed, temperature, and humidity in the atmospheric surface layer or modeling the turbulent surface fluxes of sensible and latent heat over horizontally homogeneous surfaces of snow or ice requires five pieces of information. These are the roughness lengths for wind speed (z0), temperature (zT), and humidity (zQ) and the stratification corrections for the wind speed and scalar profiles m and h, respectively. Because over snow and ice the atmospheric surface layer is often stably stratified, the discussion here focuses first on which of the many suggested m and h functions to use over snow and ice. On the basis of four profile metricsthe critical Richardson number, the Deacon numbers for wind speed and temperature, and the turbulent Prandtl numberthe manuscript recommends the Holtslag and de Bruin m and h functions because these have the best properties in very stable stratification. Next, a reanalysis of five previously published datasets confirms the validity of a parameterization for zT/z0 as a function of the roughness Reynolds number (R) that the author reported in 1987. The zT/z0 data analyzed here and that parameterization are compatible for R values between 104 and 100, which span the range from aerodynamically smooth through aerodynamically rough flow. Discussion of a z0 parameterization is deffered and an insufficiency of data for evaluating zQ is reported, although some zQ data is presented. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Hydrometeorology American Meteorological Society

Parameterizing Scalar Transfer over Snow and Ice: A Review

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Publisher
American Meteorological Society
Copyright
Copyright © American Meteorological Society
ISSN
1525-7541
D.O.I.
10.1175/1525-7541(2002)003<0417:PSTOSA>2.0.CO;2
Publisher site
See Article on Publisher Site

Abstract

AbstractEvaluating the profiles of wind speed, temperature, and humidity in the atmospheric surface layer or modeling the turbulent surface fluxes of sensible and latent heat over horizontally homogeneous surfaces of snow or ice requires five pieces of information. These are the roughness lengths for wind speed (z0), temperature (zT), and humidity (zQ) and the stratification corrections for the wind speed and scalar profiles m and h, respectively. Because over snow and ice the atmospheric surface layer is often stably stratified, the discussion here focuses first on which of the many suggested m and h functions to use over snow and ice. On the basis of four profile metricsthe critical Richardson number, the Deacon numbers for wind speed and temperature, and the turbulent Prandtl numberthe manuscript recommends the Holtslag and de Bruin m and h functions because these have the best properties in very stable stratification. Next, a reanalysis of five previously published datasets confirms the validity of a parameterization for zT/z0 as a function of the roughness Reynolds number (R) that the author reported in 1987. The zT/z0 data analyzed here and that parameterization are compatible for R values between 104 and 100, which span the range from aerodynamically smooth through aerodynamically rough flow. Discussion of a z0 parameterization is deffered and an insufficiency of data for evaluating zQ is reported, although some zQ data is presented.

Journal

Journal of HydrometeorologyAmerican Meteorological Society

Published: Aug 12, 2002

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