Aerodynamic roughness height for gravel-mantled megaripples, with implications for wind profiles near TARs on Mars

Aerodynamic roughness heights of 1-3 cm were obtained from measured wind profiles collected among fields of gravel-mantled megaripples in the high desert of the Puna region of northwestern Argentina. Roughness height appears to be relatively insensitive to the angle at which the wind was incident up...

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Publicado: 2016
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00191035_v266_n_p306_Zimbelman
http://hdl.handle.net/20.500.12110/paper_00191035_v266_n_p306_Zimbelman
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spelling paper:paper_00191035_v266_n_p306_Zimbelman2023-06-08T14:40:16Z Aerodynamic roughness height for gravel-mantled megaripples, with implications for wind profiles near TARs on Mars Earth Geological processes Mars, surface Aerodynamic roughness heights of 1-3 cm were obtained from measured wind profiles collected among fields of gravel-mantled megaripples in the high desert of the Puna region of northwestern Argentina. Roughness height appears to be relatively insensitive to the angle at which the wind was incident upon the bedforms throughout the study sites. The results represent the first wind profiling measurements for large megaripples, but they also demonstrate the importance of a careful evaluation of many potential effects that can influence the utility of wind profiling data. The same effects that influence collection of fieldwork data must also be considered in any prediction of wind profiles anticipated to occur near Transverse Aeolian Ridges and other aeolian features on Mars that are intermediate in scale between wind ripples and small sand dunes. © 2015. 2016 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00191035_v266_n_p306_Zimbelman http://hdl.handle.net/20.500.12110/paper_00191035_v266_n_p306_Zimbelman
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Earth
Geological processes
Mars, surface
spellingShingle Earth
Geological processes
Mars, surface
Aerodynamic roughness height for gravel-mantled megaripples, with implications for wind profiles near TARs on Mars
topic_facet Earth
Geological processes
Mars, surface
description Aerodynamic roughness heights of 1-3 cm were obtained from measured wind profiles collected among fields of gravel-mantled megaripples in the high desert of the Puna region of northwestern Argentina. Roughness height appears to be relatively insensitive to the angle at which the wind was incident upon the bedforms throughout the study sites. The results represent the first wind profiling measurements for large megaripples, but they also demonstrate the importance of a careful evaluation of many potential effects that can influence the utility of wind profiling data. The same effects that influence collection of fieldwork data must also be considered in any prediction of wind profiles anticipated to occur near Transverse Aeolian Ridges and other aeolian features on Mars that are intermediate in scale between wind ripples and small sand dunes. © 2015.
title Aerodynamic roughness height for gravel-mantled megaripples, with implications for wind profiles near TARs on Mars
title_short Aerodynamic roughness height for gravel-mantled megaripples, with implications for wind profiles near TARs on Mars
title_full Aerodynamic roughness height for gravel-mantled megaripples, with implications for wind profiles near TARs on Mars
title_fullStr Aerodynamic roughness height for gravel-mantled megaripples, with implications for wind profiles near TARs on Mars
title_full_unstemmed Aerodynamic roughness height for gravel-mantled megaripples, with implications for wind profiles near TARs on Mars
title_sort aerodynamic roughness height for gravel-mantled megaripples, with implications for wind profiles near tars on mars
publishDate 2016
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00191035_v266_n_p306_Zimbelman
http://hdl.handle.net/20.500.12110/paper_00191035_v266_n_p306_Zimbelman
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