Aeolian processes shape landscapes on Earth and other planets, from degradation of drylands to dynamic coastal foredunes and the formation and evolution of diverse aeolian bedforms. Windblown sediment transport and resulting landforms are inherently complex. Aeolian geomorphology responds to climatic and other environmental changes and often involves interactions with other geomorphic processes. Aeolian landforms preserve records of these changes in sedimentary strata, as seen in preserved dunes on Earth and Mars. Recent advances in high‑resolution spatial and temporal datasets have enabled new analytical approaches, modeling techniques, and interdisciplinary insights. These advances present opportunities for improved management of aeolian landscapes on Earth and for deepening our understanding of planetary surface processes across the solar system. This session seeks research contributions that explore the different realms of aeolian processes, with the goal of showcasing connections and interactions across time periods and spanning various spatial and temporal scales to enhance cross-disciplinary collaboration.