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  • Anderson, F. S., R. Greeley, P. Xu, E. Lo, D. G. Blumberg, R. M. Haberle, and J. R. Murphy (1999), Assessing the Martian surface distribution of aeolian sand using a Mars general circulation model, J. Geophys. Res., 104(E8), 18,99119,002.
  • Bandfield, J. L., V. E. Hamilton, and P. R. Christensen (2000), A global view of Martian surface compositions from MGS-TES, Science, 287, 16261630.
  • Barnouin-Jha, O. S., P. H. Schultz, and J. Lever (1999), Investigating the interactions between an atmosphere and an ejecta curtain: 2. Numerical experiments, J. Geophys. Res., 104, 27,11727,132.
  • Blumberg, D. G., and R. Greeley (1996), General circulation models, J. Climatol., 9, 32483259.
  • Bourke, M. C., S. A. Wilson, and J. R. Zimbelman (2003), The variability of transverse aeolian ridges in troughs on Mars, Lunar Planet. Sci., XXXIV, abstract 2090.
  • Bourke, M. C., M. Balme, and J. R. Zimbelman (2004), A comparative analysis of barchan dunes in the intra-crater dune fields and the North Polar Sand Sea, Lunar Planet. Sci., XXXV, abstract 1453.
  • Bowen, A. J., and D. Lindley (1977), A wind-tunnel investigation of the wind speed and turbulence characteristics close to the ground over various escarpment shapes, Boundary Layer Meteorol., 12, 259271.
  • Bullard, J. E., and D. J. Nash (2000), Valley-marginal sand dunes in the south-west Kalahari: Their nature, classification and possible origins, J. Arid Environ., 45, 369383.
  • Bullard, J. E., G. F. S. Wiggs, and D. J. Nash (2000), Experimental study of wind directional variability in the vicinity of a model valley, Geomorphology, 35, 127143.
  • Calkin, P. E., and R. H. Rutford (1974), The sand dunes of Victoria Valley, Antarctica, Geogr. Rev., 64(2), 189216.
  • Carr, M. H., and M. C. Malin (2000), Meter-scale characteristics of Martian channels and valleys, Icarus, 146(2), 366386.
  • Cooke, R. U., A. Warren, and A. S. Goudie (1993), Desert Geomorphology, UCL, London.
  • Edgett, K. S. (2002), Low-albedo surfaces and eolian sediment: Mars Orbiter Camera views of western Arabia Terra craters and wind streaks, J. Geophys. Res., 107(E6), 5038, doi:10.1029/2001JE001587.
  • Edgett, K. S., and M. C. Malin (2000), New views of Mars eolian activity, materials, and surface properties: Three vignettes from the Mars Global Surveyor Mars Orbiter Camera, J. Geophys. Res., 105(E1), 16231650.
  • Fenton, L. K., J. L. Bandfield, and A. W. Ward (2003), Aeolian processes in Proctor Crater on Mars: Sedimentary history as analyzed from multiple data sets, J. Geophys. Res., 108(E12), 5129, doi:10.1029/2002JE002015.
  • Fergason, R. L., and P. R. Christensen (2002), Relationship between small scale surface features and thermal inertia units, Lunar Planetary Sci., XXXIII, abstract 1778.
  • Ferziger, J. H., and M. Pervic (1996), Computational Methods for Fluid Dynamics, 356 pp., Springer-Verlag, New York.
  • Garvey, B., G. F. S. Wiggs, I. P. Castro, and J. E. Bullard (2002), Wind tunnel and field investigation of flow dynamics within and around a valley, in International Congress of Aeolian Research, edited by J. Lee, and T. M. Zobeck, pp. 2934, Tex. Tech. Univ., Lubbock.
  • Greeley, R., and J. D. Iversen (1985), Wind as a Geological Process on Earth, Mars, Venus and Titan, 333 pp., Cambridge Univ. Press, New York.
  • Greeley, R., N. Lancaster, S. Lee, and P. Thomas (1992), Martian aeolian processes, sediments, and features, in Mars, edited by H. H. Kieffer et al., pp. 730766, Univ. of Ariz. Press, Tucson.
  • Greeley, R., N. T. Bridges, R. O. Kuzmin, and J. E. Laity (2002), Terrestrial analogs to wind-related features at the Viking and Pathfinder landing sites on Mars, J. Geophys. Res., 107(E1), 5005, doi:10.1029/2000JE001481.
  • Hiesinger, H., and J. W. Head III (2004), The Syrtis Major volcanic province, Mars: Synthesis from Mars Global Surveyor data, J. Geophys. Res., 109, E01004, doi:10.1029/2003JE002143.
  • Howard, A. H. (1985), Interaction of sand transport with topography with local winds in the northern Peruvian coastal desert, in International Workshop on the Physics of Blown Sand, edited by O. E. Barndorff-Nielsen et al., pp. 511544, Univ. of Aarhus, Aarhus, Denmark.
  • Lancaster, N. (1986), Grain size characteristics of linear dunes in the south-western Kalahari, J. Sediment. Petrol., 56, 395400.
  • Lancaster, N. (1996), Field studies of sand patch initiation processes on the northern margin of the Namib sand sea, Earth Surf. Processes Landforms, 21(10), 947954.
  • Lancaster, N., and R. Greeley (1990), Sediment volume in the North Polar sand seas of Mars, J. Geophys. Res., 95, 10,92110,927.
  • Lancaster, N., and V. Tchakerian (1996), Geomorphology and sediments of sand ramps in the Mojave Desert, Geomorphology, 17, 151165.
  • Lee, P., and P. Thomas (1995), Longitudinal dunes on Mars: Relation to current wind regimes, J. Geophys. Res., 100(E3), 53815395.
  • Li, S., X. Liu, Y. Wang, H. Jin, Q. Wang, G. Dong, J. Shen, and P. Yang (1999), Formation mechanism and development pattern of aeolian sand landforms in Yarlung Zangbo River valley, Sci. China, D42, 272284.
  • Liu, X. W., S. Li, and J. Y. Shen (1999), Wind tunnel simulation experiment of mountain dunes, J. Arid Environ., 42, 4959.
  • Mabbutt, J. A., and R. A. Wooding (1983), Analysis of longitudinal dune patterns in the northwestern Simpson Desert, central Australia, Z. Geomorphol. Suppl., 15, 5169.
  • Malin, M. C., and K. S. Edgett (2001), The Mars Global Surveyor Mars Orbiter Camera: Interplanetary cruise through primary mission, J. Geophys. Res., 106(E10), 23,42923,570.
  • Malin, M. C., et al. (1998), Early views of the Martian surface from Mars Orbiter Camera on Mars Global Surveyor, Science, 279, 16811685.
  • McKenna Neumann, C. (2004), Effects of temperature and humidity upon the transport of sedimentary particles by wind, Sedimentology, 51(1), 117.
  • Mustard, J. F., and C. D. Cooper (2002), Comparison of ISM reflectance and TES emissivity measurements of Mars, Lunar Planet. Sci., XXXIII, abstract 1979.
  • Nallasamy, M. (1985), A critical evaluation of various turbulence models as applied to internal fluid flows, NASA Tech. Pap. 2474.
  • Pelkey, S. M., B. M. Jakosky, and M. T. Mellon (2001), Thermal inertia of crater-related wind streaks on Mars, J. Geophys. Res., 106(E10), 23,90923,920.
  • Schaber, G. G., and C. S. Breed (1999), The importance of SAR wavelength in penetrating blow sand in northern Arizona, Remote Sens. Environ., 69, 87104.
  • Seppala, M. (1993), Climbing and falling sand dunes in Finnish Lapland, in The Dynamics and Environmental Context of Aeolian Sedimentary Systems, edited by K. Pye, Geol. Soc. Spec Publ., 72, 269274.
  • Sierputowski, P., J. Ostrowski, and A. Cenedese (1995), Experimental study of wind flow over the model of a valley, J. Wind Eng. Ind. Aerodyn., 57, 127136.
  • Steidtmann, J. R. (1973), Ice and snow in eolian sand dunes of southwestern Wyoming, Science, 179(4075), 796798.
  • Sullivan, R., R. Greeley, M. Kraft, G. Wilson, M. Golombek, K. Herkenhoff, J. Murphy, and P. Smith (2000), Results of the Imager for Mars Pathfinder windsock experiment, J. Geophys. Res., 105(E10), 24,54724,562.
  • Thomas, D. S. G. (1997), Arid Zone Geomorphology: Process, Form and Change in Drylands, pp. 713, John Wiley, New York.
  • Thomas, P., J. Veverka, S. Lee, and A. Bloom (1981), Classification of wind streaks on Mars, Icarus, 45, 124153.
  • Thomas, P. C., et al. (1999), Bright dunes on Mars, Nature, 397, 592594 .
  • Tsoar, H., R. Greeley, and A. R. Peterfreund (1979), Mars: The north polar sand sea and related wind patterns, J. Geophys. Res., 84, 81678180.
  • Veverka, J., P. Gierasch, and P. Thomas (1981), Wind streaks on Mars: Meteorological control of occurrence and mode of formation, Icarus, 45, 154166.
  • Wasson, R. J. (1984), Late Quaternary paleoenvironments in the desert dunefields of Australia, in Late Cainozoic Paleoclimates of the Southern Hemisphere, edited by J. C. Vogel, pp. 419432, A. A Balkema, Brookfield, Vt.
  • Wasson, R. J., and R. Hyde (1983), Factors determining desert dune types, Nature, 304, 337339.
  • White, B. R., and H. Tsoar (1998), Slope effect on saltation over a climbing sand dune, Geomorphology, 22, 159180.
  • White, F. M. (1986), Fluid Mechanics, 732 pp., McGraw-Hill, New York.
  • Whiteman, C. D., and J. C. Doran (1993), The relationship between overlying synoptic-scale flows and winds within a valley, J. Appl., 16691682.
  • Wiggs, G. F. S., I. Livingstone, and A. Warren (1996), The role of streamline curvature in sand dune dynamics: Evidence from field and wind tunnel measurements, Geomorphology, 17(1–3), 2946.
  • Wiggs, G. F. S., J. E. Bullard, B. Garvey, and I. Castro (2002), Interactions between airflow and valley topography with implications for aeolian sediment transport, Physical Geogr., 21(5), 366380.
  • Wilson, I. G. (1972), Aeolian bedforms—Their development and origins, Sedimentology, 19, 173210.
  • Wilson, I. G. (1973), Ergs, Sediment. Geol, 10, 77106.
  • Zimbelman, J. R. (1986), Surface properties of the Pettit wind streak on Mars: Implications for sediment transport, Icarus, 66, 8393.
  • Zimbelman, J. R. (2000), Non-active dunes in the Acheron Fossae region of Mars between the Viking and Mars Global Surveyor eras, Geophys. Res. Lett., 27(7), 10691072.
  • Zimbelman, J. R., and S. Wilson (2002), Ripples and dunes in the Syrtis Major region of Mars, as revealed in MOC images, Lunar Planet. Sci., XXXIII, abstract 1514.