Results 11 to 20 of about 1,738,277 (218)

Evidence of Secondary Bedform Controls on River Dune Migration

open access: yesGeophysical Research Letters
In rivers worldwide, multiple scales of dunes coexist. It is unknown how the larger, primary dunes interact with secondary bedforms that are superimposed.
J. Y. Zomer, A. J. F. Hoitink
doaj   +3 more sources

An analytical model for the growth and migration of a transverse dune

open access: yesThe European Physical Journal E, 2019
The growth and migration speed formulae for a 2-d transverse dune are derived under the assumptions of shape similarity, the near surface airflow independent of height, and the 100% sand trapping efficiency of lee face during dune evolution. Although very simple, this analytical model can quantificationally reflect the field investigations of barchan ...
Wen-Xiao, Ning   +2 more
openaire   +3 more sources

3D airflow modelling and dune migration patterns in an arid coastal dune field

open access: yesJournal of Coastal Research, 2013
0 ...
Jackson, Derek W.T.   +3 more
openaire   +3 more sources

Ecological studies of isopoda and diplopoda in dune grassland [PDF]

open access: yes, 1978
Distribution, population dynamics, biomass and population production of macrodecomposers have been studied in order to clarify the role of four species in the processes of energy transfer in a dune grassland ecosystem.
Davis, Robert Clive
core   +7 more sources

Strong-wind events control barchan dune migration

open access: yesCommunications Earth & Environment
Wind is the most important external force in shaping aeolian landforms. Yet, it remains unclear what role the strong-wind events will play in the development of aeolian landforms compared with the effect of regular winds.
Hongjing Ren   +5 more
doaj   +2 more sources

Observation of density segregation inside migrating dunes [PDF]

open access: yesPhysical Review E, 2011
Spatiotemporal patterns in nature, such as ripples or dunes, formed by a fluid streaming over a sandy surface show complex behavior despite their simple forms. Below the surface, the granular structure of the sand particles is subject to self-organization processes, exhibiting such phenomena as reverse grading when larger particles are found on top of ...
Groh, Christopher   +2 more
openaire   +5 more sources

Dynamics of migrating sand dunes interacting with obstacles [PDF]

open access: yesPhysical Review Fluids, 2021
Wind- and water-driven migrating sand dunes frequently interact with elevated natural and artificial topographical features. The dune-obstacle interaction can alter the migrating behavior of the dune and, depending on the nature of the obstacle, it may generate various societal and technological risks.
Karol A. Bacik   +4 more
openaire   +2 more sources

The role of long-term landscape photography as a tool in dune management [PDF]

open access: yes, 2009
Attitudes to maintaining dune diversity are changing under the realization that existing dune stabilization techniques are fixing dune landscapes, causing ‘coastal squeeze’ and loss of habitat as shorelines retreat.
Worsley, Annie T.   +7 more
core   +2 more sources

Sand dunes as migrating strings

open access: yesPhysical Review E, 2013
We develop a reduced complexity model for three-dimensional sand dunes, based on a simplified description of the longitudinal and lateral sand transport. The spatiotemporal evolution of a dune migrating over a nonerodible bed under unidirectional wind is reduced to the dynamics of its crest line, providing a simple framework for the investigation of ...
Guignier, Lucie   +4 more
openaire   +4 more sources

Change detection, risk assessment and mass balance of mobile dune fields near Dunhuang Oasis with optical imagery and global terrain datasets

open access: yesInternational Journal of Digital Earth, 2020
Quantifying the kinematic evolution patterns of dune migration plays a major role in resisting the sand-dust disasters and evaluating the desertification process. With the increment of optical observations, measuring the dune migration with dense spatial
Chao Ding   +3 more
doaj   +1 more source

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