arXiv (All)
open access
A windy sea surface with Stokes waves
Predicting the transition of wind-forced, gravito-capillary surface waves from smooth to corrugated states remains a longstanding problem in nonlinear surface wave mechanics. Solving driven-dissipative, nonlinear potential flow equations we map these waves ($4-13$ cm) onto a Reynolds number -- wave
Conceptio Open Archive
Analyze & explore related research in Conceptio
Connect this record directly into your research workflow or AI agent. Explore citations across open repositories, query full text, and export structured proof bundles.
This document is indexed with metadata only: full text is not available in the archive for this record. Open the official source ↗
Related documents
- A Computational investigation on the dynamics of shallow water waves#956559
- A numerical model for the effect of ocean waves on the adjacent airflow#668707
- Surface gravity wave-mean flow interaction with comparable spatial scales. Part I: reduced wave equations#999105
- Existence and stability of capillary-gravity wave-borne vortices#1077718
- Measuring Ocean Surface Waves#460835
Record · ID 927409
Retrieved via Conceptio: every document is proof-bundled with source, license, and retrieval metadata.
Retrieved via Conceptio: every document is proof-bundled with source, license, and retrieval metadata.
Bring this data into your agent: Connect via MCP or API · 20 free credits to start · no card required
Read the Docs → · View CLI source on GitHub · Conceptio Open Knowledge Archive
Read the Docs → · View CLI source on GitHub · Conceptio Open Knowledge Archive