ON THE STEADY-STATE FLOW OF SEA ICE.
Abstract
The purpose of this paper is to create a model in which the ice and ocean are viewed as a dynamic unit and in which the gradient currents and internal ice stresses are included. Also, this paper is concerned with the solution of such a model.
Document Details
- Document Type
- Technical Report
- Publication Date
- Jul 01, 1964
- Accession Number
- AD0604368
Entities
People
- William Joseph Campbell
Organizations
- University of Washington