Abstract
The processes that initiate and sustain sediment transport which contribute to the modification of aeolian deposits in Mars’ low-density atmosphere are still not fully understood despite recent atmospheric modelling. However, detailed microscale wind flow modelling, using Computational Fluid Dynamics at a resolution of
| Original language | English |
|---|---|
| Article number | e0276547 |
| Number of pages | 24 |
| Journal | PLoS One |
| Volume | 17 |
| Issue number | 11 |
| DOIs | |
| Publication status | Published - 4 Nov 2022 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 9 Industry, Innovation, and Infrastructure
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SDG 13 Climate Action
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