Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Xinghui Huo"'
Publikováno v:
Frontiers in Physics, Vol 9 (2021)
A sand surface subjected to a continuous wind field exhibits a regular ripple surface. These aeolian sand ripples emerge and develop under the coupling effect between the wind field, bed surface topology, and sand particle transportation. Lots of the
Externí odkaz:
https://doaj.org/article/28c34be6debc49a3a25499ab285310f6
Publikováno v:
Journal of Geophysical Research. Earth Surface. Apr2024, Vol. 129 Issue 4, p1-15. 15p.
Publikováno v:
Processes; Volume 10; Issue 2; Pages: 354
Theoretically, the sand flux will not change after the wind-driven sand particle transport reaches the saturated state. However, it has been found in many wind-tunnel experiments that the sand flux will gradually decrease with time in long-term parti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7ca25a2dcf6593c2689d3f398a7b113b
Publikováno v:
Journal of Geophysical Research: Earth Surface. 124:2311-2321
Reliably predicting the geomorphology and climate of planetary bodies requires knowledge of the dynamic threshold wind shear velocity below which saltation transport ceases. Here we measure this threshold in a wind tunnel for four well-sorted and two
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::21defb46f75bcfb718d8aee96e939953
https://doi.org/10.1029/2019jf005094
https://doi.org/10.1029/2019jf005094
Publikováno v:
Frontiers in Physics, Vol 9 (2021)
A sand surface subjected to a continuous wind field exhibits a regular ripple surface. These aeolian sand ripples emerge and develop under the coupling effect between the wind field, bed surface topology, and sand particle transportation. Lots of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0d0217c3e3fb88ffadda41f2b5d4a407
https://www.frontiersin.org/articles/10.3389/fphy.2021.662389/full
https://www.frontiersin.org/articles/10.3389/fphy.2021.662389/full