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Morphodynamic study of reticulate dunes at southeastern fringe of the Tengger Desert

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Abstract

Reticulate dunes are one of the commonest dune types, and yet the least understood. Reticulate dunes at southeastern Tengger Desert are constituted by NE-SW trending primary ridges and nearly vertical secondary ridges. The result of field work studying the morphodynamics and formation mechanism for reticulate dunes in this area shows that the primary ridges were formed by dominant northwest wind and the secondary ridges developed and maintained by alternating dominant wind and subdominant northeast wind on the basis of the primary ridges. Viewed from morphodynamics, reticulate dunes correspond to the complex transverse dune on which the longitudinal element superimposed.

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Authors and Affiliations

  1. Institute of Desert Research, Chinese Academy of Sciences, 730000, Lanzhou, China

    Si Ha, Guangrong Dong & Guiyong Wang

  2. Xi’an State Key Laboratory of Loess and Quaternary Geology, Chinese Academy of Sciences, 710054, Xi’an, China

    Si Ha, Guangrong Dong & Guiyong Wang

Authors
  1. Si Ha
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  2. Guangrong Dong
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  3. Guiyong Wang
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Additional information

Project supported by the National Natural Science Foundation of China (Grant No. NSFC-49501001).

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Ha, S., Dong, G. & Wang, G. Morphodynamic study of reticulate dunes at southeastern fringe of the Tengger Desert. Sci. China Ser. D-Earth Sci. 42, 207–215 (1999). https://doi.org/10.1007/BF02878520

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  • DOI: https://doi.org/10.1007/BF02878520

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