An integrated model for dune morphology and sand fluxes on Mars
详细信息 查看全文
- 作者：K.D. Runyona ; kirby.runyon@gmail.com" class="auth_mail" title="E-mail the corresponding author ; N.T. Bridgesb ; a ; F. Ayoubc ; C.E. Newmand ; J.J. Quadee
- 关键词：aeolian ; Mars ; climate ; stratigraphy ; surface processes ; GCM
- 刊名：Earth and Planetary Science Letters
- 出版年：2017
- 出版时间：1 January 2017
- 年：2017
- 卷：457
- 期：Complete
- 页码：204-212
- 全文大小：2781 K
文摘
- •
Mars dune fields exhibit a downwind evolution in morphology and sediment flux.
- •
Internal boundary layer theory and slope speedup explain observed sediment flux.
- •
These findings have implications for interpreting Martian stratigraphy.