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Journal articles on the topic 'Aeolian transport'

Author: Grafiati

Published: 4 June 2021

Last updated: 5 February 2022

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1

Sarre, R. D. "Aeolian sand transport." Progress in Physical Geography: Earth and Environment 11, no. 2 (1987): 157–82. http://dx.doi.org/10.1177/030913338701100201.

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2

Haanhout, Bas, Arjen Luijendijk, and Sierd De Vries. "HOW TIDES AND WAVES ENHANCE AEOLIAN SEDIMENT TRANSPORT AT THE SAND MOTOR MEGA NOURISHMENT." Coastal Engineering Proceedings, no. 36 (December 30, 2018): 74. http://dx.doi.org/10.9753/icce.v36.sediment.74.

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In this paper we will present a two-dimensional application of the Windsurf modeling framework on the Sand Motor mega-nourishment in The Netherlands that allows for detailed simulation of the interaction between subtidal and subaerial processes. Expanding knowledge concerning the close entanglement between subtidal and subaerial processes in coastal environments initiated the development of the open-source Windsurf modeling framework that enables us to simulate multi-fraction sediment transport due to subtidal and subaerial processes simultaneously. The Windsurf framework couples separate mode

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3

Schönfeldt, Hans Jürgen. "Establishing the threshold for intermittent aeolian sediment transport." Meteorologische Zeitschrift 13, no. 5 (2004): 437–44. http://dx.doi.org/10.1127/0941-2948/2004/0013-0437.

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4

Hage, Pam, Gerben Ruessink, Zilla van Aartrijk, and Jasper Donker. "Using Video Monitoring to Test a Fetch-Based Aeolian Sand Transport Model." Journal of Marine Science and Engineering 8, no. 2 (2020): 110. http://dx.doi.org/10.3390/jmse8020110.

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Transport of beach sand to the foredune by wind is essential for dunes to grow. The aeolian sand transport rate is related to wind velocity, but wind-based models often overpredict this transport for narrow beaches (<100 m). To better predict aeolian sand transport, the fetch-based Aeolus model was developed. Here, we qualitatively test this model by comparing its transport-rate output to visual signs of aeolian transport on video imagery collected at Egmond aan Zee, the Netherlands, during a six-month winter period. The Aeolus model and the Argus images often agree on the timing of aeolian

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5

Pasini, José Miguel, and James T. Jenkins. "Aeolian transport with collisional suspension." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 363, no. 1832 (2005): 1625–46. http://dx.doi.org/10.1098/rsta.2005.1598.

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This paper considers the aeolian transport of sand by a wind so strong that the concentration of sand near the bed makes collisions between grains inevitable. It employs an improved model of such a collisional flow which includes turbulent suspension, viscous dissipation and new top boundary conditions that are validated by numerical calculations of collisionless trajectories.

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6

Selmani, Houssem, Alexandre Valance, Ahmed Ould El Moctar, Pascal Dupont, and Rabah Zegadi. "Relaxation processes in Aeolian transport." EPJ Web of Conferences 140 (2017): 03055. http://dx.doi.org/10.1051/epjconf/201714003055.

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7

Sherman, Douglas J., Bailiang Li, Jean T. Ellis, Eugene J. Farrell, Luis Parente Maia, and Helena Granja. "Recalibrating aeolian sand transport models." Earth Surface Processes and Landforms 38, no. 2 (2012): 169–78. http://dx.doi.org/10.1002/esp.3310.

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8

Bourman, R. P. "Aeolian sand transport along beaches." Australian Geographer 17, no. 1 (1986): 30–34. http://dx.doi.org/10.1080/00049188608702897.

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9

Willetts, B. "Aeolian and fluvial grain transport." Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences 356, no. 1747 (1998): 2497–513. http://dx.doi.org/10.1098/rsta.1998.0283.

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10

Livingstone, Ian. "Editorial: aeolian sand transport processes." Earth Surface Processes and Landforms 24, no. 5 (1999): 381. http://dx.doi.org/10.1002/(sici)1096-9837(199905)24:5<381::aid-esp994>3.0.co;2-t.

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11

Zhang, Pei, Douglas J. Sherman, and Bailiang Li. "Aeolian creep transport: A review." Aeolian Research 51 (May 2021): 100711. http://dx.doi.org/10.1016/j.aeolia.2021.100711.

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12

Kreslavsly, Mikhail A., and Nataliya V. Bondarenko. "Aeolian sand transport and aeolian deposits on Venus: A review." Aeolian Research 26 (June 2017): 29–46. http://dx.doi.org/10.1016/j.aeolia.2016.06.001.

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13

Reahl, Jocelyn N., Marjorie D. Cantine, Julia Wilcots, Tyler J. Mackey, and Kristin D. Bergmann. "Meta-analysis of Cryogenian through modern quartz microtextures reveals sediment transport histories." Journal of Sedimentary Research 91, no. 9 (2021): 929–44. http://dx.doi.org/10.2110/jsr.2020.151.

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ABSTRACT Quantitative analysis of quartz microtextures by means of scanning electron microscopy (SEM) can reveal the transport histories of modern and ancient sediments. However, because workers identify and count microtextures differently, it is difficult to directly compare quantitative microtextural data analyzed by different workers. As a result, the defining microtextures of certain transport modes and their probabilities of occurrence are not well constrained. We used principal-component analysis (PCA) to directly compare modern and ancient aeolian, fluvial, and glacial samples from the

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14

Nordstrom, Karl F., Nancy L. Jackson, and Katherine H. Korotky. "Aeolian Sediment Transport Across Beach Wrack." Journal of Coastal Research 59 (March 2011): 211–17. http://dx.doi.org/10.2112/si59-022.1.

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15

Jenkins, J. T., and A. Valance. "Periodic trajectories in aeolian sand transport." Physics of Fluids 26, no. 7 (2014): 073301. http://dx.doi.org/10.1063/1.4885576.

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16

Chapman, David M. "Aeolian sand transport—an optimized model." Earth Surface Processes and Landforms 15, no. 8 (1990): 751–60. http://dx.doi.org/10.1002/esp.3290150808.

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17

Stout, John E. "Detecting patterns of aeolian transport direction." Journal of Arid Environments 107 (August 2014): 18–25. http://dx.doi.org/10.1016/j.jaridenv.2014.04.001.

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18

Baddock, M. C., C. L. Strong, P. S. Murray, and G. H. McTainsh. "Aeolian dust as a transport hazard." Atmospheric Environment 71 (June 2013): 7–14. http://dx.doi.org/10.1016/j.atmosenv.2013.01.042.

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19

Valance, Alexandre, Keld Rømer Rasmussen, Ahmed Ould El Moctar, and Pascal Dupont. "The physics of Aeolian sand transport." Comptes Rendus Physique 16, no. 1 (2015): 105–17. http://dx.doi.org/10.1016/j.crhy.2015.01.006.

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20

Sun, Qicheng, and Guangqian Wang. "Numerical simulation of aeolian sediment transport." Chinese Science Bulletin 46, no. 9 (2001): 786–88. http://dx.doi.org/10.1007/bf03187224.

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21

Bogs, S. "Aeolian grain transport, vol. 1. mechanics." Sedimentary Geology 78, no. 1-2 (1992): 152–53. http://dx.doi.org/10.1016/0037-0738(92)90122-8.

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22

Trouvilliez, A., H. Gallée, F. Naaim-Bouvet, et al. "Comparison of aeolian snow transport events and snow mass fluxes between observations and simulations made by the regional climate model MAR in Adélie Land, East Antarctica." Cryosphere Discussions 8, no. 6 (2014): 6007–32. http://dx.doi.org/10.5194/tcd-8-6007-2014.

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Abstract. The regional climate model MAR including a coupled snow pack/aeolian snow transport parameterisation is compared with aeolian snow mass fluxes at a fine spatial resolution (5 km horizontally and 2 m vertically) and at a fine temporal resolution (30 min) over 1 month in Antarctica. Numerous feedbacks are taken into account in the MAR including the drag partitioning caused by the roughness elements. Wind speed is correctly simulated with a positive value of the Nash test (0.60 and 0.37) but the wind speeds above 10 m s−1 are underestimated. The aeolian snow transport events are correct

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23

Hage, Pam, Gerben Ruessink, and Jasper Donker. "Using Argus Video Monitoring to Determine Limiting Factors of Aeolian Sand Transport on a Narrow Beach." Journal of Marine Science and Engineering 6, no. 4 (2018): 138. http://dx.doi.org/10.3390/jmse6040138.

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Aeolian sediment transport on beaches is responsible for dune growth and/or recovery. Models predicting potential aeolian sediment transport rates often overpredict the amount of deposition on the foredune when applied to narrow (<100 m) beaches, pointing to supply limitations. Our goal is to better understand these limitations, especially in the long-term (>years) in order to improve predicted transport volumes and the timing of transport. Here, we used 8 years of Argus video images at Egmond aan Zee, The Netherlands, in combination with routine weather data to delineate 241 limited fro

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24

Wang, H., and X. Jia. "Selective deposition response to aeolian-fluvial sediment supply in the desert braided channel of the Upper Yellow River, China." Natural Hazards and Earth System Sciences Discussions 3, no. 2 (2015): 1269–90. http://dx.doi.org/10.5194/nhessd-3-1269-2015.

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Abstract. Rivers flow across aeolian dunes and develop braided stream channels. Both aeolian and fluvial sediment supplies regulate sediment transport and deposition in such a cross-dune braided river. Here we show a significant selective deposition in response to both aeolian and fluvial sediment supplies in the Ulan Buh desert braided channel. This selective deposition developed by the interaction between the flows and the Aeolian-fluvial sediment supplies, making the coarser sediments (> 0.08 mm) from aeolian sand supply and bank erosion to accumulate in the channel center and the finer

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25

Żmudzka, Elwira, Dariusz Woronko, and Maciej Dłużewski. "The Sources of Moisture in the Sand Dunes – The Example of the Western Sahara Dune Field." Quaestiones Geographicae 33, no. 3 (2014): 199–204. http://dx.doi.org/10.2478/quageo-2014-0042.

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Abstract Climatic and meteorological conditions may limit the aeolian transport within barchans. An explanation of that issue was the main goal of the investigation held in Western Sahara dune fields located around Tarfaya and Laâyoune. Particular attention was paid to the factors causing the moisture content rising of the sand dune surface layer, which could influence the wind threshold shear velocity in the aeolian transport. The wetted surface layer of sand, when receiving moisture from precipitation or suspensions, reduces the aeolian transport, even in case of wind velocity above 4-5 m s-

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26

Wang, H., X. Jia, Y. Li, and W. Peng. "Selective deposition response to aeolian–fluvial sediment supply in the desert braided channel of the upper Yellow River, China." Natural Hazards and Earth System Sciences 15, no. 9 (2015): 1955–62. http://dx.doi.org/10.5194/nhess-15-1955-2015.

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Abstract. Rivers flow across aeolian dunes and develop braided stream channels. Both aeolian and fluvial sediment supplies regulate sediment transport and deposition in such cross-dune braided rivers. Here we show a significant selective deposition in response to both aeolian and fluvial sediment supplies in the Ulan Buh desert braided channel. The Ulan Buh desert is the main coarse sediment source for this desert braided channel, and the mean percentage of the coarser (> 0.08 mm) grains on the aeolian dunes surface is 95.34 %. The lateral selective deposition process is developed by the in

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27

Prestedge, Gordon K., and Christopher A. Fleming. "ANALYSIS OF A BEACH QUALITY PROBLEM." Coastal Engineering Proceedings 1, no. 20 (1986): 108. http://dx.doi.org/10.9753/icce.v20.108.

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A study was recently undertaken to investigate sediment transport on a section of coastline where recreational beaches have experienced periodic erosion. Alongshore, onshore/offshore and aeolian sediment transport processes were investigated and quantitative transports predicted with the aid of calibration using surveys and aerial photographs. This paper describes the study and the recommendations proposed for beach quality improvements.

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28

Wan, Shiming, Youbin Sun, and Kana Nagashima. "Asian dust from land to sea: processes, history and effect from modern observation to geological records." Geological Magazine 157, no. 5 (2020): 701–6. http://dx.doi.org/10.1017/s0016756820000333.

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AbstractProduction, transport and deposition of aeolian dust from land to sea closely interact with regional environment and global climate. This Special Issue addresses transport of aeolian dust from the Asian inland to the Loess Plateau and North Pacific Ocean and their possible links to oceanic ecosystem, global climate and even human activity, over various timescales. The papers in this volume are multidisciplinary in nature and include sedimentology, mineralogy, geochemistry, environmental magnetism and climate modelling on multi-timescales from interannual, glacial–interglacial to tecton

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29

Dong, Zhibao, Xiaoping Liu, Hongtao Wang, and Xunming Wang. "Aeolian sand transport: a wind tunnel model." Sedimentary Geology 161, no. 1-2 (2003): 71–83. http://dx.doi.org/10.1016/s0037-0738(02)00396-2.

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30

Kang, Liqiang, and Liejin Guo. "Eulerian–Lagrangian simulation of aeolian sand transport." Powder Technology 162, no. 2 (2006): 111–20. http://dx.doi.org/10.1016/j.powtec.2005.12.002.

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31

Bauer, Bernard O., and Robin G. D. Davidson-Arnott. "Aeolian particle flux profiles and transport unsteadiness." Journal of Geophysical Research: Earth Surface 119, no. 7 (2014): 1542–63. http://dx.doi.org/10.1002/2014jf003128.

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32

Jackson and Cooper. "Beach fetch distance and aeolian sediment transport." Sedimentology 46, no. 3 (1999): 517–22. http://dx.doi.org/10.1046/j.1365-3091.1999.00228.x.

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33

Sørensen, Michael. "On the rate of aeolian sand transport." Geomorphology 59, no. 1-4 (2004): 53–62. http://dx.doi.org/10.1016/j.geomorph.2003.09.005.

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34

van Boxel, J. H., G. Sterk, and S. M. Arens. "Sonic anemometers in aeolian sediment transport research." Geomorphology 59, no. 1-4 (2004): 131–47. http://dx.doi.org/10.1016/j.geomorph.2003.09.011.

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35

Swann, C., and D. J. Sherman. "A bedload trap for aeolian sand transport." Aeolian Research 11 (December 2013): 61–66. http://dx.doi.org/10.1016/j.aeolia.2013.09.003.

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36

de Vries, S., J. S. M. van Thiel de Vries, L. C. van Rijn, S. M. Arens, and R. Ranasinghe. "Aeolian sediment transport in supply limited situations." Aeolian Research 12 (March 2014): 75–85. http://dx.doi.org/10.1016/j.aeolia.2013.11.005.

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37

Poortinga, Ate, Hans van Rheenen, Jean T. Ellis, and Douglas J. Sherman. "Measuring aeolian sand transport using acoustic sensors." Aeolian Research 16 (March 2015): 143–51. http://dx.doi.org/10.1016/j.aeolia.2014.12.003.

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38

Williams, Isaac A., Kathelijne M. Wijnberg, and Suzanne J. M. H. Hulscher. "Detection of aeolian transport in coastal images." Aeolian Research 35 (December 2018): 47–57. http://dx.doi.org/10.1016/j.aeolia.2018.09.003.

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39

Dong, ZhiBao, Ping Lv, ZhengCai Zhang, and JunFeng Lu. "Aeolian transport over a developing transverse dune." Journal of Arid Land 6, no. 3 (2013): 243–54. http://dx.doi.org/10.1007/s40333-013-0243-2.

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40

Rasmussen, Keld R., and Michael Sørensen. "Aeolian mass transport near the saltation threshold." Earth Surface Processes and Landforms 24, no. 5 (1999): 413–22. http://dx.doi.org/10.1002/(sici)1096-9837(199905)24:5<413::aid-esp997>3.0.co;2-i.

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41

Duarte-Campos, Leonardo, Kathelijne Wijnberg, and Suzanne Hulscher. "Estimating Annual Onshore Aeolian Sand Supply from the Intertidal Beach Using an Aggregated-Scale Transport Formula." Journal of Marine Science and Engineering 6, no. 4 (2018): 127. http://dx.doi.org/10.3390/jmse6040127.

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In this paper, we explore an approach for annual-scale transport prediction from the intertidal beach, in which we aggregate the surface conditions of the intertidal beach, in particular moisture content and roughness, and use hourly monitoring data of wind speed and wind direction. For our case study area (Egmond Beach, The Netherlands), we include Argus video imagery in our analysis to assess the occurrence of aeolian sand transport. With the approach described to determine a characteristic moisture content value for aeolian transport, we obtained surface moisture values of 1.2% to 3.2% for

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42

Bazhenova, Olga, Dmitrii Kobylkin, and Elizaveta Tyumentseva. "Aeolian Material Migration in Transbaikalia (Asian Russia)." Geosciences 9, no. 1 (2019): 41. http://dx.doi.org/10.3390/geosciences9010041.

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We revealed regional features of functioning of a large Transbaikalian aeolian morphodynamic system. Natural pre-conditions, current realities and factors of development of aeolian processes are investigated. The paper considers regularities of spatial distribution of deflation, transit, and aeolian accumulation zones. Main directions of aeolian migration of matter are determined. Pulsating nature of aeolian processes development in Holocene has been established. Identified are intrasecular cycles and Holocene dynamics of aeolian processes. We identified intrasecular (11, 27–35 years old), sec

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43

Strypsteen, Houthuys, and Rauwoens. "Dune Volume Changes at Decadal Timescales and Its Relation with Potential Aeolian Transport." Journal of Marine Science and Engineering 7, no. 10 (2019): 357. http://dx.doi.org/10.3390/jmse7100357.

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Long-term changes in dune volume at the Belgian coast are analyzed based on measured data by airborne surveys available from 1979. For most of the 65 km long coastal stretch, dune volume increases linearly in time at a constant rate. Dune growth varies between 0–12.3 m³/m/year with an average dune growth of 6.2 m³/m/year, featuring large variations in longshore directions. Based on a wind data set from 2000–2017, it is found that potential aeolian sediment transport has its main drift from the west to southwest direction (onshore to oblique onshore). Based on a modified Bagnold model, onshore

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44

Hesse, Ralf. "Using remote sensing to quantify aeolian transport and estimate the age of the terminal dune field Dunas Pampa Blanca in southern Peru." Quaternary Research 71, no. 3 (2009): 426–36. http://dx.doi.org/10.1016/j.yqres.2009.02.002.

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AbstractAeolian dunes are widely used to reconstruct paleoenvironmental conditions. However, terminal dune fields (ergs) in the coastal desert of southern Peru – where information regarding Quaternary paleoenvironmental conditions is very limited – have until now not been used for paleoenvironmental reconstructions and the time depth of their accumulation is unknown. Here, different estimates are derived to constrain the time depth recorded in the Dunas Pampa Blanca, a terminal dune field in coastal southern Peru. Dune field age is calculated using the volume of the Dunas Pampa Blanca and (i)

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45

Stauch, Georg. "A conceptual model for the interpretation of aeolian sediments from a semiarid high-mountain environment since the late glacial." Quaternary Research 91, no. 1 (2018): 24–34. http://dx.doi.org/10.1017/qua.2018.35.

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AbstractDifferent interpretations of accumulation and preservation of aeolian sediments lead to divergent and sometimes contradictory palaeoclimate reconstructions. Although aeolian transport mainly occurs during dry climate, the preservation of the aeolian sediment is a critical factor in many environments in determining the nature of the aeolian sedimentary archive. Analysis of more than 200 optically stimulated luminescence ages for aeolian sands from Tibet shows four different aeolian phases of accumulation. Strong aeolian activity occurred during the last glacial maximum, but hardly any a

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46

Trouvilliez, Alexandre, Florence Naaim-Bouvet, Hervé Bellot, Christophe Genthon, and Hubert Gallée. "Evaluation of the FlowCapt Acoustic Sensor for the Aeolian Transport of Snow." Journal of Atmospheric and Oceanic Technology 32, no. 9 (2015): 1630–41. http://dx.doi.org/10.1175/jtech-d-14-00104.1.

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AbstractFlowCapt acoustic sensors, designed for measuring the aeolian transport of snow fluxes, are compared to the snow particle counter S7optical sensor, considered herein as the reference. They were compared in the French Alps at the Lac Blanc Pass, where a bench test for the aeolian transport of snow was set up. The two existing generations of FlowCapt are compared. Both seem to be good detectors for the aeolian transport of snow, especially for transport events with a flux above 1 g m−2 s−1. The second-generation FlowCapt is also compared in terms of quantification. The aeolian snow mass

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47

Delgado-Fernandez, Irene, and Robin Davidson-Arnott. "Meso-scale aeolian sediment input to coastal dunes: The nature of aeolian transport events." Geomorphology 126, no. 1-2 (2011): 217–32. http://dx.doi.org/10.1016/j.geomorph.2010.11.005.

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48

Jia, Xiaopeng, and Haibing Wang. "Element Geochemical Analysis of the Contribution of Aeolian Sand to Suspended Sediment in Desert Stream Flash Floods." Scientific World Journal 2014 (2014): 1–12. http://dx.doi.org/10.1155/2014/620610.

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The interaction of wind and water in semiarid and arid areas usually leads to low-frequency flash flood events in desert rivers, which have adverse effects on river systems and ecology. In arid zones, many aeolian dune-fields terminate in stream channels and deliver aeolian sand to the channels. Although aeolian processes are common to many desert rivers, whether the aeolian processes contribute to fluvial sediment loss is still unknown. Here, we identified the aeolian-fluvial cycling process responsible for the high rate of suspended sediment transport in the Sudalaer desert stream in the Ord

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49

Sherman, Zhang, Martin, et al. "Aeolian Ripple Migration and Associated Creep Transport Rates." Geosciences 9, no. 9 (2019): 389. http://dx.doi.org/10.3390/geosciences9090389.

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Wind-formed ripples are distinctive features of many sandy aeolian environments, and their development and migration are basic responses to sand transport via saltation. Using data from the literature and from original field experiments, we presented empirical models linking dimensionless migration rates, urgd (ur is the ripple migration speed, g is the gravity acceleration, and d is the grain diameter) with dimensionless shear velocity, u*/u*t (u* is shear velocity and u*t is fluid threshold shear velocity). Data from previous studies provided 34 usable cases from four wind tunnel experiments

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50

ANDREOTTI, BRUNO. "A two-species model of aeolian sand transport." Journal of Fluid Mechanics 510 (July 10, 2004): 47–70. http://dx.doi.org/10.1017/s0022112004009073.

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