SEARCH

SEARCH BY CITATION

References

  • Alexandrov, Y., J. B. Laronne, and I. Reid (2003), Suspended sediment concentration and its variation with water discharge in a dryland ephemeral channel, northern Negev, Israel, J. Arid Environ., 53, 7384.
  • Amit, R., and R. Gerson (1986), The evolution of Holocene Reg (gravelly) soils in deserts—An example from the Dead Sea region, Catena, 13, 5979.
  • Anderson, K., S. Wells, and R. Graham (2002), Pedogenesis of vesicular horizons, Cima Volcanic field, Mojave Desert, California, Soil Sci. Soc. Am. J., 66, 878887.
  • Bacon, S. N., E. V. McDonald, T. G. Caldwell, and G. K. Dalldorf (2010), Timing and distribution of alluvial fan sedimentation in response to strengthening of late Holocene ENSO variability in the Sonoran Desert, southwestern Arizona, USA, Quat. Res., 73, 425438.
  • Birkeland, P. W. (1999), Soils and Geomorphology, Oxford University Press, New York.
  • Blackwelder, E. (1931), The lowering of playas by deflation, Am. J. Sci., 21, 140144.
  • Bullard, J. E., G. McTainsh, and C. Pudmenzky (2007), Factors affecting the nature and rate of dust production from natural dune sands, Sedimentology, 54, 169182.
  • Cahill, T. A., T. E. Gill, J. S. Reid, E. A. Gearhart, and D. A. Gillette (1996), Saltating particles, playa crusts and dust aerosols at Owens (dry) Lake, California, Earth Surf. Processes Landforms, 21, 621639.
  • Chadwick, O. A., and J. O. Davis (1990), Soil-forming intervals caused by eolian sediment pulses in the Lahontan basin, northwestern Nevada, Geology, 18, 243246.
  • Clarke, M. L., and H. M. Rendell (1998), Climate change impacts on sand supply and the formation of desert sand dunes in the south-west U.S.A., J. Arid Environ., 39, 517531.
  • Crouvi, O., R. Amit, Y. Enzel, N. Porat, and A. Sandler (2008), Sand dunes as a major proximal dust source for late Pleistocene loess in the Negev desert, Israel, Quat. Res., 70, 275282.
  • Crouvi, O., K. Schepanski, R. Amit, A. R. Gillespie, and Y. Enzel (2012), Multiple dust source in the Sahara Desert: the importance of sand dunes, Geophys. Res. Lett., 39, L13401 doi:10.1029/2012GL052145.
  • Dohrenwend, J. C., and R. S. U. Smith (1991), Quaternary geology and tectonics of the Salton Trough, in Quaternary Nonglacial Geology: Conterminous U.S., pp. 334337, edited by R. B. Morrison, Geological Society of America, Boulder, Colorado.
  • El-Sayed, M. I. (1999), Sedimentological characteristics and morphology of the aeolian sand dunes in the eastern part of the UAE: A case study from Ar Rub' Al Kahli, Sed. Geol., 123, 219238.
  • Ely, L. L., Y. Enzel, V. R. Baker, and D. R. Cayan (1993), A 5000-year record of extreme floods and climate change in the southwestern United States, Science, 262, 410412.
  • Enzel, Y., R. Amit, O. Crouvi, and N. Porat (2010), Abrasion-derived sediments under intensified winds at the latest Pleistocene leading edge of the advancing Sinai-Negev erg, Quat. Res., 74, 121131.
  • Folk, R. L. (1955), Student operator error in determination of roundness, sphericity, and grain size, J. Sed. Pet., 25, 297301.
  • Gerson, R., and R. Amit (1987), Rates and modes of dust accretion and deposition in an arid region—The Negev, Israel, in Desert Sediments: Ancient and Modern, Geol. Soc. London Special Publications no. 35, edited by L. Frostick, and I. Reid, pp. 157169, Blackwell, Oxford.
  • Ginoux, P., M. Chin, I. Tegen, J. Prospero, B. Holben, O. Dubovik, and S.-J. Lin (2001), Sources and global distributions of dust aerosols simulated with the GOCART model, J. Geophys. Res., 106, 20,25520,273, doi:10.1029/2000JD000053.
  • Gill, T. E. (1996), Eolian sediment generated by anthropogenic disturbance of playas: Human impacts on the geomorphic system and geomorphic impacts on the human system, Geomorphology, 17, 207228.
  • Gillette, D. A., J. Adams, A. Endo, D. Smith, and R. Kihl (1980), Threshold velocities for input of soil particles into the air by desert soils, J. Geophys. Res., 85, 56215630.
  • Goldstein, H. L., R. L. Reynolds, M. C. Reheis, J. C. Yount, and J. C. Neff (2008), Compositional trends in aeolian dust along a transect across the southwestern United States, J. Geophys. Res., 113, F02S02, doi:10.1029/2007JF000751.
  • Gomes, L., G. Bergametti, G. Coudé-Gaussen, and P. Rognon (1990), Submicron desert dusts: A sandblasting process, J. Geophys. Res., 95(D9), 13,92713,935, doi:10.1029/JD095iD09p13927.
  • Goudie, A. S. (2002), Great Warm Deserts of the World: Landscape and Evolution, Oxford University Press, Oxford.
  • Goudie, A. S., and N. J. Middleton (2006), Desert Dust in the Global System, Springer, Berlin.
  • Graham, R. C., D. R. Hirmas, Y. A. Wood, and C. Amrhein (2008), Large near-surface nitrate pools in soils capped by desert pavement in the Mojave Desert, California, Geology, 36, 259262.
  • Gutiérrez, M. (2001), Climatic Geomorphology, Elsevier, Amsterdam.
  • Hamerlynck, E. P., J. R. McAuliffe, E. V. McDonald, and S. D. Smith (2002), Impacts of desert soil processes and drought on contrasting Mojave Desert shrubs, Ecology, 83, 768779.
  • Helm, P. J., and C. S. Breed (1999), Instrumented field studies of sediment transport by wind, in Desert Winds: Monitoring wind-related surface processes in Arizona, New Mexico, and California, U.S. Geol. Survey Prof. Paper no. 1598, edited by C. S. Breed and M. C. Reheis, pp. 3154, US Government Printing Office, Washington.
  • Huggett, R. J. (2007), Fundamentals of Geomorphology, 2nd ed., Routledge, London.
  • Jackson, M. L. (2005), Soil Chemical Analysis: Advanced Course, 2nd ed., Univ. Wisconsin-Madison Libraries Parallel Press, Madison.
  • Johnson, D. M., P. R. Hooper, and R. M. Conrey (1999), XRF analysis of rocks and minerals for major and trace elements on a single low dilution Li-tetraborate fused bead, Adv. X Ray Anal., 41, 843867.
  • Khalaf, F. I., and I. M. Gharib (1985), Roundness parameters of quartz grains of Recent aeolian sand deposits in Kuwait, Sed. Geol., 45, 147158.
  • Kuenen, P. H. (1960), Experimental abrasion 4: Eolian action, J. Geol., 68, 427449.
  • Lancaster, N., and V. P. Tchakerian (1996), Geomorphology and sediments of sand ramps in the Mojave Desert, Geomorphology, 17, 151165.
  • Lancaster, N., and V. P. Tchakerian (2003), Late Quaternary eolian dynamics, Mojave Desert, California, Geol. Soc. Am. Special Paper, 368, 231249.
  • Langford, R. P. (1989), Fluvial-eolian interactions: Part I, modern systems, Sedimentology 36, 10231035.
  • Mahowald, N. M., R. G. Bryant, J. del Corral, and L. Steinberger (2003), Ephemeral lakes and desert dust sources, Geophys. Res. Lett., 30, 1074, doi:10.1029/2002GL016041.
  • Marx, S. K., B. S. Kamber, and H. A. McGowan (2005), Provenance of long-traveled dust determined with ultra-trace-element composition: A pilot study with samples from New Zealand glaciers, Earth Surf. Processes Landforms, 30, 699716.
  • McAuliffe, J. R., and E. V. McDonald (1995), A piedmont landscape in the eastern Mojave Desert: Examples of linkages between biotic and physical components, San Bernardino County Mus. Assoc. Q., 42, 5363.
  • McDonald, E. V. (1994), The relative influences of climate change, desert dust, and lithological control on soil-geomorphic processes and hydrology of calcic soils formed on Quaternary alluvial-fan deposits in the Mojave Desert, California, Ph.D. thesis, Univ. of N. M., Albuquerque, NM.
  • McDonald, E. V. (2002), Numerical simulations of soil water balance in support of revegetation of damaged military lands in arid regions, Arid Land Res. Management, 16, 277291.
  • McDonald, E. V., L. D. McFadden, and S. G. Wells (1995), The relative influences of climate change, desert dust, and lithologic control on soil-geomorphic processes on alluvial fans, Mojave Desert, California, San Bernardino County Mus. Assoc. Q., 42, 3542.
  • McDonald, E. V., F. B. Pierson, G. N. Flerchinger, and L. D. McFadden (1996), Application of a soil-water balance model to evaluate the influence of Holocene climate change on calcic soils, Mojave Desert, California, U.S.A., Geoderma, 74, 167192.
  • McDonald, E. V., L. D. McFadden, and S. G. Wells (2003), Regional response of alluvial fans to the Pleistocene-Holocene climatic transition, Mojave Desert, California, Geol. Soc. Am. Special Paper, 368, 189205.
  • McFadden, L. D., S. G. Wells, and J. C. Dohrenwend (1986), Influences of Quaternary change on processes of soil development on desert loess deposits of the Cima volcanic field, California, Catena, 13, 361389.
  • McFadden, L. D., S. G. Wells, and M. J. Jercinovich (1987), Influences of eolian and pedogenic processes on the origin and evolution of desert pavements, Geology, 15, 504508.
  • McFadden, L. D., S. G. Wells, W. J. Brown, and Y. Enzel (1992), Soil genesis on beach ridges of pluvial Lake Mojave—Implications for Holocene lacustrine and eolian events in the Mojave Desert, southern California, Catena, 19, 7797.
  • McFadden, L. D., E. V. McDonald, S. G. Wells, K. Anderson, J. Quade, and S. L. Forman (1998), The vesicular layer and carbonate collars of desert soils and pavements: Formation, age and relation to climate change, Geomorphology, 24, 101145.
  • McFadden, L. D., M. C. Eppes, A. R. Gillespie, and B. Hallet (2005), Physical weathering in arid landscapes due to diurnal variation in the direction of solar heating, Geol. Soc. Am. Bull., 117, 161173.
  • Michalski, G., J. K. Bohlke, and M. Thiemens (2004), Long term atmospheric deposition as the source of nitrate and other salts in the Atacama Desert, Chile: New evidence from mass-independent oxygen isotopic compositions, Geochim. Cosmochim. Acta, 68, 40234038.
  • Miller, D. E. (1971), Formation of vesicular structure in soil, Soil Sci. Soc. Am. Proc., 35, 635637.
  • Miller, D. M., K. M. Schmidt, S. A. Mahan, J. P. McGeehin, L. A. Owen, J. A. Barron, F. Lehmkhul, and R. Lohrer (2010), Holocene landscape response to seasonality of storms in the Mojave Desert, Quat. International, 215, 4561.
  • Muhs, D. R., and J. B. Benedict (2006), Eolian additions to late Quaternary alpine soils, Indian Peaks Widerness Area, Colorado Front Range, Arctic, Antarctic, Alpine Res., 38, 120130.
  • Muhs, D. R., C. A. Bush, S. D. Cowherd, and S. Mahan (1995), Geomorphic and geochemical evidence for the source of sand in the Algodones dunes, Colorado Desert, southeastern California, in Desert Aeolian Processes, edited by V. P. Tchakerian, pp. 3474, Chapman and Hall, London.
  • Muhs, D. R., R. L. Reynolds, J. Been, and G. Skipp (2003), Eolian sand transport pathways in the southwestern United States: Importance of the Colorado River and local sources, Quat. International, 104, 318.
  • Muhs, D. R., E. A. Bettis III, J. N. Aleinikoff, J. P. McGeehin, J. Beann, G. Skipp, B. D. Marshall, H. M. Roberts, W. C. Johnson, and R. Benton (2008a), Origin and paleoclimatic significance of late Quaternary loess in Nebraska: Evidence from stratigraphy, chronology, sedimentology, and geochemistry, Geol. Soc. Am. Bull., 120, 13781407.
  • Muhs, D. R., J. R. Budahn, D. L. Johnson, M. Reheis, J. Beann, G. Skipp, E. Fisher, and J. A. Jones (2008b), Geochemical evidence for airborne dust additions to soils in Channel Islands National Park, California, Geol. Soc. Am. Bull., 120, 106126.
  • Nalpanis, P. (1985), Saltating and suspended particles over flat and sloping surfaces. 2. Experiments and numerical simulations, Proc. Int. Workshop Physics Blown Sand, Aarhaus Univ., Univ. Aarhus Mem. 8, 3766.
  • Okin, G. S., and M. C. Reheis (2002), An ENSO predictor of dust emission in the southwestern United States, Geophys. Res. Lett., 29(9), doi:10.1029/2001GL014494.
  • Okin, G. S., J. E. Bullard, R. L. Reynolds, J.-A. C. Ballantine, K. Schepanski, M. C. Todd, J. Belnap, M. C. Baddock, T. E. Gill, and M. E. Miller (2011), Dust: Small-scale processes with global consequences, Eos Trans. AGU, 92(29), 241, doi:10.1029/2011EO290001.
  • Pease, P. P., and V. P. Tchakerian (2003), Geochemistry of sediment from Quaternary sand ramps in the southeastern Mojave Desert, California, Quat. International, 104, 1929.
  • Pelletier, J. D., and J. P. Cook (2005), Deposition of playa windblown dust over geologic time scales, Geology, 33, 909912.
  • Peterson, F. F. (1981), Landforms of the Basin and Range province defined for soil survey, Nevada Agricultural Experiment Station Tech. Bull. 28, Univ. Nevada Reno.
  • Powell, D. M., I. Reid, J. B. Laronne, and L. E. Frostick (1996), Bedload as a component of sediment yield from a semiarid watershed of the northern Negev, in Erosion and Sediment Yield: Global and Regional Perspectives, Internat. Assoc. Hydrological Sci. Pub. no. 236, pp. 389397, IAHS Press, Wallingford.
  • Powers, M. C. (1953), A new roundness scale for sedimentary particles, J. Sed. Petrology, 23, 117119.
  • Prospero, J. M., P. Ginoux, O. Torres, S. E. Nicholson, and T. E. Gill (2002), Environmental characterization of global sources of atmospheric soil dust identified with the Nimbus 7 Total Ozone Mapping Spectrometer (TOMS) absorbing aerosol product, Rev. Geophys., 40(1), 1002, doi:10.1029/2000RG000095.
  • Pye, K. (1987), Aeolian Dust and Dust Deposits, Elsevier, New York.
  • Quick, D. J., and O. A. Chadwick (2011), Accumulation of salt-rich dust from Owens Lake playa in nearby alluvial soils, Aeolian Res., 3, 2329.
  • Ramsey, M. S., P. R. Christensen, N. Lancaster, and D. A. Howard (1999), Identification of sand sources and transport pathways at the Kelso Dunes, California, using thermal infrared remote sensing, Geol. Soc. Am. Bull., 111, 646662.
  • Reheis, M. C. (2006), A 16-year record of eolian dust in southern Nevada and California, USA: Controls on dust generation and accumulation, J. Arid Environ., 67, 487520.
  • Reheis, M. C., and R. Kihl (1995), Dust deposition in southern Nevada and California, 1984–1989: Relations to climate, source area, and source lithology, J. Geophys. Res., 100, 88938918, doi:10.1029/94JD03245.
  • Reheis, M. C., J. W. Harden, L. D. McFadden, and R. R. Shroba (1989), Development rates of late Quaternary soils: Silver Lake Playa, California, Soil Sci. Soc. Am. J., 53, 11271140.
  • Reheis, M. C., J. M. Sowers, E. M. Taylor, L. D. McFadden, and J. W. Harden (1992), Morphology and genesis of carbonate soils on the Kyle Canyon fan, Nevada, USA, Geoderma, 52, 303342.
  • Reheis, M. C., J. C. Goodmacher, J. W. Harden, L. D. McFadden, T. K. Rockwell, R. R. Shroba, J. M. Sowers, and E. M. Taylor (1995), Quaternary soils and dust deposition in southern Nevada and California, Geol. Soc. Am. Bull., 107, 10031022.
  • Reheis, M. C., J. R. Budahn, and P. J. Lamothe (2002), Geochemical evidence for diversity of dust sources in the southwestern United States, Geochim. Cosmochim. Acta, 66, 15691587.
  • Reheis, M. C., J. R. Budahn, P. J. Lamothe, and R. L. Reynolds (2009), Compositions of modern dust and surface sediments in the Desert Southwest, United States, J. Geophys. Res., 114, F01028, doi:10.1029/2008JF001009.
  • Reynolds, R. L., M. Reheis, J. Yount, and P. Lamothe (2006), Composition of aeolian dust in natural traps on isolated surfaces of the central Mojave Desert—Insights to mixing, sources, and nutrient inputs, J. Arid Environ., 66, 4261.
  • Reynolds, R. L., J. C. Yount, M. Reheis, H. Goldstein, P. Chavez, R. Fulton, J. Whitney, C. Fuller, and R. Forester (2007), Dust emission from wet and dry playas in the Mojave Desert, USA, Earth Surface Proc. Landforms, 32, 18111827.
  • Shafer, D. S., M. H. Young, S. F. Zitzer, T. G. Caldwell, and E. V. McDonald (2007), Impacts of interrelated biotic and abiotic processes during the past 125,000 years of landscape evolution in the Northern Mojave Desert, Nevada, USA, J. Arid Environ., 69, 633657.
  • Shao, Y., M. R. Raupach, and P. A. Findlater (1993), Effect of saltation bombardment on the entrainment of dust by wind, J. Geophys. Res., 98, 12,71912,726, doi:10.1029/93JD00396.
  • Spencer, J. E., and P. J. Patchett (1997), Sr isotope evidence for a lacustrine origin for the upper Miocene to Pliocene Bouse Formation, lower Colorado River trough, and implications for timing of Colorado Plateau uplift, Geol. Soc. Am. Bull., 109, 767778.
  • Sun, J. (2002), Provenance of loess material and formation of loess deposits on the Chinese Loess Plateau, Earth Planetary Sci. Lett., 203, 845859.
  • Sweeney, M. R., D. R. Gaylord, and A. J. Busacca (2007), The evolution of Eureka Flat: A dust-producing engine of the Palouse loess, USA, Quat. International, 162–163, 7696.
  • Sweeney, M. R., E. V. McDonald, and V. Eytemezian (2011), Quantifying dust emissions from desert landforms, eastern Mojave Desert, USA, Geomorphology, 135, 2134.
  • Taylor, S. R., and S. M. McLennan (1985), The Continental Crust: Its composition and evolution, Blackwell Scientific, Oxford.
  • Tchakerian, V. P., and N. Lancaster (2002), Late Quaternary arid/humid cycles in the Mojave Desert and western Great Basin of North America, Quat. Sci. Rev., 21, 799810.
  • Tegen, I. (2003), Modeling the mineral dust aerosol cycle in the climate system, Quat. Sci. Rev., 22, 18211834.
  • Tegen, I., S. P. Harrison, K. Kohfeld, I. C. Prentice, M. Coe, and M. Heimann (2002), Impact of vegetation and preferential source areas on global dust aerosol: Results from a model study, J. Geophys. Res., 107(D21), 4576, doi:10.1029/2001JD000963.
  • Thomas, D. S. G. (2000), Arid Zone Geomorphology, Wiley, Chichester.
  • Tsoar, H., and K. Pye (1995), Dust transport and the question of desert loess formation, Sedimentology, 34, 139153.
  • Valentine, G. A., and C. D. Harrington (2006), Clast size controls and longevity of Pleistocene desert pavements at Lathrop Wells and Red Cone volcanoes, southern Nevada, Geology, 34, 533536.
  • VanCuren, R., and T. Cahill (2002), Asian aerosols in North America: Frequency and concentration of fine dust, J. Geophys. Res., 107(D24), 4804 doi: 10.1029/2002JD002204.
  • Washington, R., and M. C. Todd (2005), Atmospheric controls on mineral dust emission from the Bodélé Depression, Chad: The role of the low level jet, Geophys. Res. Lett., 32, L17701, doi: 10.1029/2005GL023597.
  • Waters, M. R. (1983), Late Holocene lacustrine chronology and archaeology of ancient Lake Cahuilla, California, Quat. Res., 19, 373387.
  • Wells, S. G., J. C. Dohrenwend, L. D. McFadden, B. D. Turrin, and K. D. Mahrer (1985), Late Cenozoic landscape evolution on lava flow surfaces of the Cima volcanic field, Mojave Desert, California, Geol. Soc. Am. Bull., 96, 15181529.
  • Wells, S. G., L. D. McFadden, and J. C. Dohrenwend (1987a), Influence of late Quaternary climatic changes on geomorphic and pedogenic processes on a desert piedmont, Eastern Mojave Desert, California, Quat. Res., 27, 130146.
  • Wells, S. G., L. D. McFadden, and M. J. Jercinovich (1987b), Influences of eolian and pedogenic processes on the origin and evolution of desert pavements, Geology, 15, 504508.
  • Wells, S. G., L. D. McFadden, J. Poths, and C. T. Olinger (1995), Cosmogenic He-3 surface-exposure dating of stone pavements—Implications for landscape evolution in deserts, Geology, 23, 613616.
  • Wood, Y. A., R. C. Graham, and S. G. Wells (2005), Surface control of desert pavement pedologic process and landscape function, Cima volcanic field, Mojave Desert, California, Catena, 59, 205230.
  • Yaalon, D. H. and E. Ganoor (1973), The influence of dust on soils during the Quaternary, Soil Sci., 116, 146155.
  • Young, J. A., and R. A. Evans (1986), Erosion and deposition of fine sediments from playas, J. Arid Environ., 10, 103115.
  • Young, M. H., E. V. McDonald, T. G. Caldwell, S. G. Brenner, and D. G. Meadows (2004), Hydraulic properties of a desert soil chronosequence in the Mojave Desert, USA, Vadose Zone J., 3, 956963.
  • Zimbelman, J. R., S. H. Williams, and V. P. Tchakerian, (1995), Sand transport paths in the Mojave Desert, southwestern United States, in Desert Aeolian Processes, edited by V. P. Tchakerian, pp. 101129, Chapman and Hall, London.
  • Zimbelman, J. R., and S. H. Williams (2002), Geochemical indicators of separate sources for eolian sands in the eastern Mojave Desert, California, and western Arizona, Geol. Soc. Am. Bull., 114, 490496.
  • Zlotnik, V. A., J. B. Ong, J. D. Lenters, J. Schmeider, and S. C. Fritz (2012), Quantification of salt dust pathways from a groundwater-fed lake: Implications for solute budgets and dust emission rates, J. Geophys. Res., 117, F02014, doi:10.1029/2011JF002107.