Dune fields often exhibit complex patterns of vegetation and morphology over relatively short distances. An analysis of the White Sands dune field in New Mexico attributes the shift in dune form to the development of an internal boundary layer over the rough dune-field surface.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 12 print issues and online access
$259.00 per year
only $21.58 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Derickson, D., Kocurek, G., Ewing, R. C. & Bristow, C. Geomorphology 99, 186–204 (2008).
Jerolmack, D. J. et al. Nature Geosci. 5, 206–209 (2012).
Garratt, J. R. Bound-Lay. Meteorol. 50, 171–203 (1990).
White, F. M. Viscous Fluid Flow 2nd edn (McGraw-Hill, 1991)
Bagnold, R. A. The Physics of Blown Sand and Desert Dunes (Methuen, 1941).
Kocurek, G. et al. Sedim. Geol. 197, 313–331 (2007).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Rasmussen, K. Flow and form. Nature Geosci 5, 164–165 (2012). https://doi.org/10.1038/ngeo1408
Published:
Issue Date:
DOI: https://doi.org/10.1038/ngeo1408