Wind Speed, Stability and Eddy Viscosity over Melting Ice Surfaces

Abstract The laws of wind-speed variation with height and their modification with stability are discussed and applied to observations in the first 2 m. over various cold surfaces. An exponential law is superior save in frequent, near-neutral conditions, but the logarithmic law is superior in neutral...

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Published in:Journal of Glaciology
Main Authors: Grainger, M. E., Lister, H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1966
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000019109
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019109
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spelling crcambridgeupr:10.1017/s0022143000019109 2024-09-15T18:15:37+00:00 Wind Speed, Stability and Eddy Viscosity over Melting Ice Surfaces Grainger, M. E. Lister, H. 1966 http://dx.doi.org/10.1017/s0022143000019109 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019109 en eng Cambridge University Press (CUP) Journal of Glaciology volume 6, issue 43, page 101-127 ISSN 0022-1430 1727-5652 journal-article 1966 crcambridgeupr https://doi.org/10.1017/s0022143000019109 2024-07-10T04:04:24Z Abstract The laws of wind-speed variation with height and their modification with stability are discussed and applied to observations in the first 2 m. over various cold surfaces. An exponential law is superior save in frequent, near-neutral conditions, but the logarithmic law is superior in neutral and again in really stable conditions. A power law and a logarithmic-plus-linear law give the best fit with the data only at moderate stabilities. A logarithmic-plus-cubic law of wind speed is evolved that permits suppression of linear additions to the logarithmic law at two distinct stabilities. A power form of variation of Richardson number with height is found and compared with a linear form. The former is applied with the logarithmicplus-cubic law to the observed data, though with limited success. Eddy-viscosity coefficients for the different laws are compared. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 6 43 101 127
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The laws of wind-speed variation with height and their modification with stability are discussed and applied to observations in the first 2 m. over various cold surfaces. An exponential law is superior save in frequent, near-neutral conditions, but the logarithmic law is superior in neutral and again in really stable conditions. A power law and a logarithmic-plus-linear law give the best fit with the data only at moderate stabilities. A logarithmic-plus-cubic law of wind speed is evolved that permits suppression of linear additions to the logarithmic law at two distinct stabilities. A power form of variation of Richardson number with height is found and compared with a linear form. The former is applied with the logarithmicplus-cubic law to the observed data, though with limited success. Eddy-viscosity coefficients for the different laws are compared.
format Article in Journal/Newspaper
author Grainger, M. E.
Lister, H.
spellingShingle Grainger, M. E.
Lister, H.
Wind Speed, Stability and Eddy Viscosity over Melting Ice Surfaces
author_facet Grainger, M. E.
Lister, H.
author_sort Grainger, M. E.
title Wind Speed, Stability and Eddy Viscosity over Melting Ice Surfaces
title_short Wind Speed, Stability and Eddy Viscosity over Melting Ice Surfaces
title_full Wind Speed, Stability and Eddy Viscosity over Melting Ice Surfaces
title_fullStr Wind Speed, Stability and Eddy Viscosity over Melting Ice Surfaces
title_full_unstemmed Wind Speed, Stability and Eddy Viscosity over Melting Ice Surfaces
title_sort wind speed, stability and eddy viscosity over melting ice surfaces
publisher Cambridge University Press (CUP)
publishDate 1966
url http://dx.doi.org/10.1017/s0022143000019109
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019109
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 6, issue 43, page 101-127
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000019109
container_title Journal of Glaciology
container_volume 6
container_issue 43
container_start_page 101
op_container_end_page 127
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