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. 2017 Dec 7;122(12):2510–2543. doi: 10.1002/2017JE005267

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©2017. The Authors.

This is an open access article under the terms of the Creative Commons Attribution‐NonCommercial‐NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made.

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In situ measurements of aeolian sands were made at and near High dune. (a) A portion of a color Mastcam mosaic (from mcam05350; sol 1171) near High dune, showing targets Warsaw, the crest of a large ripple, and Weissrand, a rover wheel track through the sand (inset context image is a Navcam mosaic from sol 1181). Portions of MAHLI focus merge images of targets (b) Warsaw (natural illumination; 1182MH0005380000402862R00) and (c) Weissrand (natural illumination; 1182MH0005380000402830R00). (d) A portion of RGB color Mastcam mosaic (from mcam05372; sol 1184) on the stoss edge of High dune, showing targets Kibnas, a small ripple within a larger ripple trough, and Barby, the crest of a ripple (inset context image is a Navcam from sol 1184). Portions of MAHLI focus merge images of (e) Kibnas (night with white LED illumination; 1184MH0001630000402965R00) and (f) Barby (natural illumination; 1184MH0001630000402969R00). MAHLI products used are the dark‐subtracted, flat‐fielded, DRXX level processed data at resolutions in Table 2.