Results 161 to 170 of about 590 (205)

Sediment Source Fingerprinting of the Lake Urmia Sand Dunes. [PDF]

Sci Rep, 2018
Ahmady-Birgani H, Agahi E, Ahmadi SJ, Erfanian M.   +3 more
europepmc   +1 more source

Sand Dune Encroachment and Desertification Processes of the Rigboland Sand Sea, Central Iran. [PDF]

Sci Rep, 2017
Ahmady-Birgani H, McQueen KG, Moeinaddini M, Naseri H.   +3 more
europepmc   +1 more source

Phase diagrams of dune shape and orientation depending on sand availability. [PDF]

Sci Rep, 2015
Gao X, Narteau C, Rozier O, Courrech du Pont S.   +3 more
europepmc   +1 more source

Size distribution of barchan dunes by a coarse-grained dune model

NCTAM papers, National Congress of Theoretical and Applied Mechanics, Japan, 2008
openaire   +1 more source

Dust, sand and wind drive slope streaks on Mars. [PDF]

Nat Commun
Bickel VT.
europepmc   +1 more source

Wind-Driven Erosion and Exposure Potential at Mars 2020 Rover Candidate-Landing Sites. [PDF]

J Geophys Res Planets, 2018
Chojnacki M, Banks M, Urso A.
europepmc   +1 more source

Boundary condition controls on the high-sand-flux regions of Mars. [PDF]

Geology, 2019
Chojnacki M, Banks ME, Fenton LK, Urso AC.   +3 more
europepmc   +1 more source

Numerical modeling of the wind flow over a transverse dune. [PDF]

Sci Rep, 2013
Araújo AD, Parteli EJ, Pöschel T, Andrade JS, Herrmann HJ.   +4 more
europepmc   +1 more source

Hydrodynamic significance of variable ripple morphology across deep-water barchan dunes in the Faroe–Shetland Channel

Marine Geology, 2002
A combination of high-resolution (30 kHz) sidescan sonar and seafloor photography has been used to image barchan dunes and sand ripples in the Faroe-Shetland Channel.
Russell B Wynn, Douglas G Masson, Brian J Bett   +2 more
exaly   +2 more sources

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A continuous model for sand dunes: Review, new developments and application to barchan dunes and barchan dune fields

Earth Surface Processes and Landforms, 2010
AbstractBasically, sand dunes are patterns resulting from the coupling of hydrodynamic and sediment transport. Once grains move, they modify the surface topography which in turns modifies the flow. This important feedback mechanism lies at the core of continuous dune modelling.
Orencio Duran, Eric J R Parteli, Hans J Herrmann   +2 more
exaly   +2 more sources