The rate of granule ripple movement on Earth and Mars

dc.contributor.authorZimbelman, James R.
dc.contributor.authorIrwin, Rossman P., III
dc.contributor.authorWilliams, Steven H.
dc.contributor.authorBunch, Fred
dc.contributor.authorValdez, Andrew
dc.contributor.authorStevens, Scott
dc.date.accessioned2009-09-04T18:12:59Z
dc.date.available2009-09-04T18:12:59Z
dc.date.issued2009
dc.description.abstractThe rate of movement for 3- and 10-cm-high granule ripples was documented in September of 2006 at Great Sand Dunes National Park and Preserve during a particularly strong wind event. Impact creep induced by saltating sand caused ~24 granules min-1 to cross each cm of crest length during wind that averaged ~9 m s-1 (at a height well above 1 m), which is substantially larger than the threshold for saltation of sand. Extension of this documented granule movement rate to Mars suggests that a 25-cm-high granule ripple should require from hundreds to thousands of Earth-years to move 1 cm under present atmospheric conditions.
dc.format.extent542834 bytes
dc.format.extent71–76
dc.format.mimetypeapplication/pdf
dc.identifier0019-1035
dc.identifier.citationZimbelman, James R., Irwin, Rossman P., III, Williams, Steven H., Bunch, Fred, Valdez, Andrew, and Stevens, Scott. 2009. "<a href="https://repository.si.edu/handle/10088/8076">The rate of granule ripple movement on Earth and Mars</a>." <em>Icarus</em>, 203, (1) 71–76. <a href="https://doi.org/10.1016/j.icarus.2009.03.033">https://doi.org/10.1016/j.icarus.2009.03.033</a>.
dc.identifier.issn0019-1035
dc.identifier.urihttp://hdl.handle.net/10088/8076
dc.language.isoen_US
dc.relation.ispartofIcarus 203 (1)
dc.titleThe rate of granule ripple movement on Earth and Mars
dc.typearticle
sro.description.unitNASM
sro.description.unitNASM-CEPS
sro.identifier.doi10.1016/j.icarus.2009.03.033
sro.identifier.itemID79923
sro.identifier.refworksID101546
sro.identifier.urlhttps://repository.si.edu/handle/10088/8076

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