Estimating aerodynamic roughness over complex surface terrain
Estimating aerodynamic roughness over complex surface terrain
Surface roughness plays a key role in determining aerodynamic roughness length (zo) and shear velocity, both of which are fundamental for determining wind erosion threshold and potential. Whilst zo can be quantified from wind measurements, large proportions of wind erosion prone surfaces remain too remote for this to be a viable approach. Alternative approaches therefore seek to relate zo to morphological roughness metrics. However, dust emitting landscapes typically consist of complex small-scale surface roughness patterns and few metrics exist for these surfaces which can be used to predict zo for modelling wind erosion potential. In this study terrestrial laser scanning was used to characterise the roughness of typical dust emitting surfaces (playa and sandar) where element protrusion heights ranged from 1 to 199?mm, over which vertical wind velocity profiles were collected to enable estimation of zo. Our data suggest that, although a reasonable relationship (R^2?>?0.79) is apparent between 3D roughness density and zo, the spacing of morphological elements is far less powerful in explaining variations in zo than metrics based on surface roughness height (R^2?>?0.92). This finding is in juxtaposition to wind erosion models that assume the spacing of larger-scale isolated roughness elements is most important in determining zo. Rather, our data show that any metric based on element protrusion height has a higher likelihood of successfully predicting zo. This finding has important implications for the development of wind erosion and dust emission models that seek to predict the efficiency of aeolian processes in remote terrestrial and planetary environments
aerodynamic roughness, surface roughness, terrestrial laser scanning (TLS), wind erosion, spectral analysis, sediment entrainment
12948-12961
Nield, Joanna M.
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King, James
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Wiggs, Giles F.S.
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Leyland, Julian
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Bryant, Robert G.
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Chiverrell, Richard C.
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Darby, Stephen E.
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Eckardt, Frank D.
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Thomas, David S.G.
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Vircavs, Larisa H.
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Washington, Richard
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24 December 2013
Nield, Joanna M.
173be2c5-b953-481a-abc4-c095e5e4b790
King, James
12837388-21db-49a1-b806-5c46fd9afac6
Wiggs, Giles F.S.
0b574ec8-fcd5-43b8-8b0b-0c84a01499d4
Leyland, Julian
6b1bb9b9-f3d5-4f40-8dd3-232139510e15
Bryant, Robert G.
b6405ac1-d101-4921-ac6a-3ae02940493e
Chiverrell, Richard C.
193e87d2-aae0-499c-b92b-af07eb2a494d
Darby, Stephen E.
4c3e1c76-d404-4ff3-86f8-84e42fbb7970
Eckardt, Frank D.
7110a4b9-5338-48be-a1f4-f3b85b47c37b
Thomas, David S.G.
55cf7c36-c6fe-4c2f-b771-424e29f72b9f
Vircavs, Larisa H.
f8b97cec-e61f-465a-a655-dfad69940da9
Washington, Richard
9c257ee6-a5ec-4c1f-b977-efef444901a2
Nield, Joanna M., King, James, Wiggs, Giles F.S., Leyland, Julian, Bryant, Robert G., Chiverrell, Richard C., Darby, Stephen E., Eckardt, Frank D., Thomas, David S.G., Vircavs, Larisa H. and Washington, Richard
(2013)
Estimating aerodynamic roughness over complex surface terrain.
Journal of Geophysical Research: Atmospheres, 118, .
(doi:10.1002/2013JD020632).
Abstract
Surface roughness plays a key role in determining aerodynamic roughness length (zo) and shear velocity, both of which are fundamental for determining wind erosion threshold and potential. Whilst zo can be quantified from wind measurements, large proportions of wind erosion prone surfaces remain too remote for this to be a viable approach. Alternative approaches therefore seek to relate zo to morphological roughness metrics. However, dust emitting landscapes typically consist of complex small-scale surface roughness patterns and few metrics exist for these surfaces which can be used to predict zo for modelling wind erosion potential. In this study terrestrial laser scanning was used to characterise the roughness of typical dust emitting surfaces (playa and sandar) where element protrusion heights ranged from 1 to 199?mm, over which vertical wind velocity profiles were collected to enable estimation of zo. Our data suggest that, although a reasonable relationship (R^2?>?0.79) is apparent between 3D roughness density and zo, the spacing of morphological elements is far less powerful in explaining variations in zo than metrics based on surface roughness height (R^2?>?0.92). This finding is in juxtaposition to wind erosion models that assume the spacing of larger-scale isolated roughness elements is most important in determining zo. Rather, our data show that any metric based on element protrusion height has a higher likelihood of successfully predicting zo. This finding has important implications for the development of wind erosion and dust emission models that seek to predict the efficiency of aeolian processes in remote terrestrial and planetary environments
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Published date: 24 December 2013
Keywords:
aerodynamic roughness, surface roughness, terrestrial laser scanning (TLS), wind erosion, spectral analysis, sediment entrainment
Organisations:
Earth Surface Dynamics
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Local EPrints ID: 359930
URI: http://eprints.soton.ac.uk/id/eprint/359930
ISSN: 2169-8996
PURE UUID: 6819bfed-b2b2-458d-8f12-67d07fa515d1
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Date deposited: 21 Nov 2013 09:10
Last modified: 15 Mar 2024 03:29
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Contributors
Author:
James King
Author:
Giles F.S. Wiggs
Author:
Robert G. Bryant
Author:
Richard C. Chiverrell
Author:
Frank D. Eckardt
Author:
David S.G. Thomas
Author:
Larisa H. Vircavs
Author:
Richard Washington
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