Morphological change and migration of revegetated dunes in the Ketu Sandy Land of the Qinghai Lake, China-Reference-Cited by-同舟云学术

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Morphological change and migration of revegetated dunes in the Ketu Sandy Land of the Qinghai Lake, China

Published:2023-07 Issue:7 Volume:15 Page:827-841
ISSN:1674-6767
Container-title:Journal of Arid Land
language:en
Short-container-title:J. Arid Land

Author:

Wu Wangyang,Zhang Dengshan,Tian Lihui,Shen Tingting,Gao Bin,Yang Dehui

Publisher

Springer Science and Business Media LLC

Subject

Management, Monitoring, Policy and Law,Earth-Surface Processes,Water Science and Technology

Link

https://link.springer.com/content/pdf/10.1007/s40333-023-0021-8.pdf

Reference48 articles.

1. Anthonsen K L, Clemmensen L B, Jensen J H. 1996. Evolution of a dune from crescentic to parabolic form in response to short-term climatic changes: Råbjerg Mile, Skagen Odde, Denmark. Geomorphology, 17(1–3): 63–77.

2. Barchyn T E, Hugenholtz C H. 2012. Predicting vegetation-stabilized dune field morphology. Geophysical Research Letters, 39: L17403, doi: https://doi.org/10.1029/2012GL052905.

3. Bhadra B K, Rehpade S B, Meena H, et al. 2019. Analysis of parabolic dune morphometry and its migration in Thar desert area, India, using high-resolution satellite data and temporal DEM. Journal of the Indian Society of Remote Sensing, 47(12): 2097–2111.

4. Bishop M A. 2010. Nearest neighbor analysis of mega-barchanoid dunes, Ar Rub’ al Khali sand sea: The application of geographical indices to the understanding of dune field self-organization, maturity and environmental change. Geomorphology, 120(3–4): 186–194.

5. Bubenzer O, Bolten A. 2008. The use of new elevation data (SRTM/ASTER) for the detection and morphometric quantification of Pleistocene megadunes (draa) in the eastern Sahara and the southern Namib. Geomorphology, 102(2): 221–231.

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