- Abstract:
-
Knowledge of the changing rate of sediment flux in space and time is essential for quantifying surface erosion and deposition in desert landscapes. While many aeolian studies have relied on time-averaged parameters such as wind velocity (U) and wind shear velocity (u.) to determine sediment flux, there is increasing field evidence that high-frequency turbulence is an important driving force behind the entrainment and transport of sand. At this scale of analysis, inertia in the saltation syste...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Publisher's version
- Files:
-
-
(pdf, 2.3mb)
-
- Publisher copy:
- 10.1016/j.geomorph.2016.12.006
-
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- Grant:
- NE/L501530/1; NER/S/A/2004/12431
- Publisher:
- Elsevier Publisher's website
- Journal:
- Geomorphology Journal website
- Volume:
- 280
- Pages:
- 108–121
- Publication date:
- 2016-12-20
- Acceptance date:
- 2016-12-09
- DOI:
- EISSN:
-
1872-695X
- ISSN:
-
0169-555X
- Pubs id:
-
pubs:665773
- URN:
-
uri:a680a5a5-4798-439a-9a6f-d77420f371bb
- UUID:
-
uuid:a680a5a5-4798-439a-9a6f-d77420f371bb
- Local pid:
- pubs:665773
- Copyright holder:
- Mayaud et al.
- Copyright date:
- 2016
- Notes:
- © 2016 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY license. Open Access funded by Natural Environment Research Council.
Journal article
Modelling aeolian sand transport using a dynamic mass balancing approach
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