Planetary-scale streak structure reproduced in high-resolution simulations of the Venus atmosphere with a low-stability layer
A planetary-scale streak structure in the Venusian lower-cloud layer was observed by the Akatsuki orbiter. Here the authors present numerical simulations that reproduce such structure and reveal that a low-stability layer, which induces baroclinic disturbances, is essential for its formation.
Uloženo v:
| Hlavní autoři: | , , , , , , , , , , , , |
|---|---|
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Portfolio
2019-01-01
|
| Edice: | Nature Communications |
| On-line přístup: | https://doi.org/10.1038/s41467-018-07919-y |
| Tagy: |
Žádné tagy, Buďte první, kdo vytvoří štítek k tomuto záznamu!
|
